GERM Reservoir Database
Development and Maintenance by the EarthRef.org Database Team

GERM Database Search Results        
Reservoir Z Element Value Median SD Low High N Unit Info Reference Source(s)
Andesites 13 Al 16.21           wt%ox Condie 1993
Andesites 13 Al 16.4           wt%ox Condie 1993
Andesites 13 Al 16.8           wt%ox Condie 1993
Andesites 13 Al 15.3           wt%ox Condie 1993
Andesites 13 Al 16.6           wt%ox Condie 1993
Andesites 13 Al 16.3           wt%ox Condie 1993
Andesites 13 Al 15.6           wt%ox Condie 1993
Andesites 56 Ba 560           ppm Condie 1993
Andesites 56 Ba 648           ppm Condie 1993
Andesites 56 Ba 650           ppm Condie 1993
Andesites 56 Ba 672           ppm Condie 1993
Andesites 56 Ba 580           ppm Condie 1993
Andesites 56 Ba 570           ppm Condie 1993
Andesites 56 Ba 511           ppm Condie 1993
Andesites 20 Ca 7.2           wt%ox Condie 1993
Andesites 20 Ca 6.8           wt%ox Condie 1993
Andesites 20 Ca 6.2           wt%ox Condie 1993
Andesites 20 Ca 6.2           wt%ox Condie 1993
Andesites 20 Ca 6.3           wt%ox Condie 1993
Andesites 20 Ca 7.1           wt%ox Condie 1993
Andesites 20 Ca 6.1           wt%ox Condie 1993
Andesites 58 Ce 49           ppm Condie 1993
Andesites 58 Ce 55           ppm Condie 1993
Andesites 58 Ce 44           ppm Condie 1993
Andesites 58 Ce 44           ppm Condie 1993
Andesites 58 Ce 42           ppm Condie 1993
Andesites 58 Ce 45           ppm Condie 1993
Andesites 58 Ce 46           ppm Condie 1993
Andesites 27 Co 47           ppm Condie 1993
Andesites 27 Co 50           ppm Condie 1993
Andesites 27 Co 20           ppm Condie 1993
Andesites 27 Co 26           ppm Condie 1993
Andesites 27 Co 31           ppm Condie 1993
Andesites 27 Co 22           ppm Condie 1993
Andesites 27 Co 35           ppm Condie 1993
Andesites 24 Cr 170           ppm Condie 1993
Andesites 24 Cr 48           ppm Condie 1993
Andesites 24 Cr 200           ppm Condie 1993
Andesites 24 Cr 42           ppm Condie 1993
Andesites 24 Cr 40           ppm Condie 1993
Andesites 24 Cr 75           ppm Condie 1993
Andesites 24 Cr 50           ppm Condie 1993
Andesites 63 Eu 1           ppm Condie 1993
Andesites 63 Eu 1.4           ppm Condie 1993
Andesites 63 Eu 1           ppm Condie 1993
Andesites 63 Eu 1.1           ppm Condie 1993
Andesites 63 Eu 1.3           ppm Condie 1993
Andesites 63 Eu 1.2           ppm Condie 1993
Andesites 63 Eu 0.85           ppm Condie 1993
Andesites   Eu/Eu* 0.74             Condie 1993
Andesites   Eu/Eu* 0.81             Condie 1993
Andesites   Eu/Eu* 0.85             Condie 1993
Andesites   Eu/Eu* 0.66             Condie 1993
Andesites   Eu/Eu* 0.78             Condie 1993
Andesites   Eu/Eu* 0.65             Condie 1993
Andesites   Eu/Eu* 0.77             Condie 1993
Andesites 26 Fe 6.3           wt%ox Condie 1993
Andesites 26 Fe 6.8           wt%ox Condie 1993
Andesites 26 Fe 6.2           wt%ox Condie 1993
Andesites 26 Fe 8.2           wt%ox Condie 1993
Andesites 26 Fe 6.5           wt%ox Condie 1993
Andesites 26 Fe 6.4           wt%ox Condie 1993
Andesites 26 Fe 7.2           wt%ox Condie 1993
Andesites 64 Gd 4.94           ppm Interpolated from Sm and Tb. Condie 1993
Andesites 64 Gd 4.15           ppm Interpolated from Sm and Tb. Condie 1993
Andesites 64 Gd 4.14           ppm Interpolated from Sm and Tb. Condie 1993
Andesites 64 Gd 4.65           ppm Interpolated from Sm and Tb. Condie 1993
Andesites 64 Gd 4.59           ppm Interpolated from Sm and Tb. Condie 1993
Andesites 64 Gd 5.17           ppm Interpolated from Sm and Tb. Condie 1993
Andesites 64 Gd 4.54           ppm Interpolated from Sm and Tb. Condie 1993
Andesites 72 Hf 4.5           ppm Condie 1993
Andesites 72 Hf 4           ppm Condie 1993
Andesites 72 Hf 4           ppm Condie 1993
Andesites 72 Hf 4           ppm Condie 1993
Andesites 72 Hf 4           ppm Condie 1993
Andesites 72 Hf 3.5           ppm Condie 1993
Andesites 72 Hf 4           ppm Condie 1993
Andesites 19 K 1.15           wt%ox Condie 1993
Andesites 19 K 1.2           wt%ox Condie 1993
Andesites 19 K 1.1           wt%ox Condie 1993
Andesites 19 K 1           wt%ox Condie 1993
Andesites 19 K 1.3           wt%ox Condie 1993
Andesites 19 K 1.2           wt%ox Condie 1993
Andesites 19 K 0.82           wt%ox Condie 1993
Andesites 57 La 23           ppm Condie 1993
Andesites 57 La 18           ppm Condie 1993
Andesites 57 La 18           ppm Condie 1993
Andesites 57 La 20           ppm Condie 1993
Andesites 57 La 20           ppm Condie 1993
Andesites 57 La 17           ppm Condie 1993
Andesites 57 La 25           ppm Condie 1993
Andesites   La[n]/Yb[n] 7.6             Condie 1993
Andesites   La[n]/Yb[n] 7.3             Condie 1993
Andesites   La[n]/Yb[n] 5.2             Condie 1993
Andesites   La[n]/Yb[n] 6.1             Condie 1993
Andesites   La[n]/Yb[n] 5.7             Condie 1993
Andesites   La[n]/Yb[n] 5.5             Condie 1993
Andesites   La[n]/Yb[n] 6.1             Condie 1993
Andesites 71 Lu 0.32           ppm Condie 1993
Andesites 71 Lu 0.3           ppm Condie 1993
Andesites 71 Lu 0.33           ppm Condie 1993
Andesites 71 Lu 0.31           ppm Condie 1993
Andesites 71 Lu 0.32           ppm Condie 1993
Andesites 71 Lu 0.32           ppm Condie 1993
Andesites 71 Lu 0.3           ppm Condie 1993
Andesites 12 Mg 3.5           wt%ox Condie 1993
Andesites 12 Mg 3.3           wt%ox Condie 1993
Andesites 12 Mg 3.7           wt%ox Condie 1993
Andesites 12 Mg 4.5           wt%ox Condie 1993
Andesites 12 Mg 3.4           wt%ox Condie 1993
Andesites 12 Mg 3.9           wt%ox Condie 1993
Andesites 12 Mg 4.6           wt%ox Condie 1993
Andesites 11 Na 3.6           wt%ox Condie 1993
Andesites 11 Na 3.8           wt%ox Condie 1993
Andesites 11 Na 3.7           wt%ox Condie 1993
Andesites 11 Na 2.8           wt%ox Condie 1993
Andesites 11 Na 3.8           wt%ox Condie 1993
Andesites 11 Na 3.8           wt%ox Condie 1993
Andesites 11 Na 3.2           wt%ox Condie 1993
Andesites 41 Nb 8           ppm Condie 1993
Andesites 41 Nb 8.5           ppm Condie 1993
Andesites 41 Nb 9           ppm Condie 1993
Andesites 41 Nb 8           ppm Condie 1993
Andesites 41 Nb 6           ppm Condie 1993
Andesites 41 Nb 8           ppm Condie 1993
Andesites 41 Nb 6.1           ppm Condie 1993
Andesites 60 Nd 21           ppm Condie 1993
Andesites 60 Nd 23           ppm Condie 1993
Andesites 60 Nd 26           ppm Condie 1993
Andesites 60 Nd 25           ppm Condie 1993
Andesites 60 Nd 24           ppm Condie 1993
Andesites 60 Nd 30           ppm Condie 1993
Andesites 60 Nd 27           ppm Condie 1993
Andesites 28 Ni 40           ppm Condie 1993
Andesites 28 Ni 100           ppm Condie 1993
Andesites 28 Ni 30           ppm Condie 1993
Andesites 28 Ni 50           ppm Condie 1993
Andesites 28 Ni 42           ppm Condie 1993
Andesites 28 Ni 50           ppm Condie 1993
Andesites 28 Ni 96           ppm Condie 1993
Andesites 15 P 0.23           wt%ox Condie 1993
Andesites 15 P 0.2           wt%ox Condie 1993
Andesites 15 P 0.22           wt%ox Condie 1993
Andesites 15 P 0.22           wt%ox Condie 1993
Andesites 15 P 0.21           wt%ox Condie 1993
Andesites 15 P 0.23           wt%ox Condie 1993
Andesites 15 P 0.18           wt%ox Condie 1993
Andesites 82 Pb 20           ppm Condie 1993
Andesites 82 Pb 20           ppm Condie 1993
Andesites 82 Pb 20           ppm Condie 1993
Andesites 82 Pb 20           ppm Condie 1993
Andesites 82 Pb 20           ppm Condie 1993
Andesites 82 Pb 20           ppm Condie 1993
Andesites 82 Pb 20           ppm Condie 1993
Andesites 37 Rb 35           ppm Condie 1993
Andesites 37 Rb 41           ppm Condie 1993
Andesites 37 Rb 33           ppm Condie 1993
Andesites 37 Rb 23           ppm Condie 1993
Andesites 37 Rb 50           ppm Condie 1993
Andesites 37 Rb 37           ppm Condie 1993
Andesites 37 Rb 27           ppm Condie 1993
Andesites 21 Sc 22           ppm Condie 1993
Andesites 21 Sc 23           ppm Condie 1993
Andesites 21 Sc 20           ppm Condie 1993
Andesites 21 Sc 20           ppm Condie 1993
Andesites 21 Sc 20           ppm Condie 1993
Andesites 21 Sc 20           ppm Condie 1993
Andesites 21 Sc 18           ppm Condie 1993
Andesites 14 Si 59.4           wt%ox Condie 1993
Andesites 14 Si 59           wt%ox Condie 1993
Andesites 14 Si 59.5           wt%ox Condie 1993
Andesites 14 Si 58.8           wt%ox Condie 1993
Andesites 14 Si 59.1           wt%ox Condie 1993
Andesites 14 Si 58.7           wt%ox Condie 1993
Andesites 14 Si 59.1           wt%ox Condie 1993
Andesites 62 Sm 4.8           ppm Condie 1993
Andesites 62 Sm 3.8           ppm Condie 1993
Andesites 62 Sm 5           ppm Condie 1993
Andesites 62 Sm 3.9           ppm Condie 1993
Andesites 62 Sm 4.5           ppm Condie 1993
Andesites 62 Sm 4.6           ppm Condie 1993
Andesites 62 Sm 5.3           ppm Condie 1993
Andesites 38 Sr 290           ppm Condie 1993
Andesites 38 Sr 320           ppm Condie 1993
Andesites 38 Sr 259           ppm Condie 1993
Andesites 38 Sr 312           ppm Condie 1993
Andesites 38 Sr 360           ppm Condie 1993
Andesites 38 Sr 315           ppm Condie 1993
Andesites 38 Sr 253           ppm Condie 1993
Andesites 73 Ta 0.53           ppm Condie 1993
Andesites 73 Ta 0.5           ppm Condie 1993
Andesites 73 Ta 0.35           ppm Condie 1993
Andesites 73 Ta 0.5           ppm Condie 1993
Andesites 73 Ta 0.5           ppm Condie 1993
Andesites 73 Ta 0.4           ppm Condie 1993
Andesites 73 Ta 0.5           ppm Condie 1993
Andesites 65 Tb 0.74           ppm Condie 1993
Andesites 65 Tb 0.77           ppm Condie 1993
Andesites 65 Tb 0.7           ppm Condie 1993
Andesites 65 Tb 0.73           ppm Condie 1993
Andesites 65 Tb 0.75           ppm Condie 1993
Andesites 65 Tb 0.69           ppm Condie 1993
Andesites 65 Tb 0.85           ppm Condie 1993
Andesites 90 Th 4.3           ppm Condie 1993
Andesites 90 Th 3.4           ppm Condie 1993
Andesites 90 Th 3.5           ppm Condie 1993
Andesites 90 Th 3           ppm Condie 1993
Andesites 90 Th 3.7           ppm Condie 1993
Andesites 90 Th 3.7           ppm Condie 1993
Andesites 90 Th 4           ppm Condie 1993
Andesites 22 Ti 0.86           wt%ox Condie 1993
Andesites 22 Ti 0.76           wt%ox Condie 1993
Andesites 22 Ti 0.88           wt%ox Condie 1993
Andesites 22 Ti 0.78           wt%ox Condie 1993
Andesites 22 Ti 0.8           wt%ox Condie 1993
Andesites 22 Ti 0.74           wt%ox Condie 1993
Andesites 22 Ti 0.95           wt%ox Condie 1993
Andesites 92 U 2           ppm Condie 1993
Andesites 92 U 1.8           ppm Condie 1993
Andesites 92 U 2           ppm Condie 1993
Andesites 92 U 2           ppm Condie 1993
Andesites 92 U 2           ppm Condie 1993
Andesites 92 U 2           ppm Condie 1993
Andesites 92 U 1.5           ppm Condie 1993
Andesites 23 V 135           ppm Condie 1993
Andesites 23 V 154           ppm Condie 1993
Andesites 23 V 140           ppm Condie 1993
Andesites 23 V 140           ppm Condie 1993
Andesites 23 V 168           ppm Condie 1993
Andesites 23 V 170           ppm Condie 1993
Andesites 23 V 132           ppm Condie 1993
Andesites 39 Y 20           ppm Condie 1993
Andesites 39 Y 22           ppm Condie 1993
Andesites 39 Y 23           ppm Condie 1993
Andesites 39 Y 20           ppm Condie 1993
Andesites 39 Y 25           ppm Condie 1993
Andesites 39 Y 20           ppm Condie 1993
Andesites 39 Y 20           ppm Condie 1993
Andesites 70 Yb 1.9           ppm Condie 1993
Andesites 70 Yb 2           ppm Condie 1993
Andesites 70 Yb 2           ppm Condie 1993
Andesites 70 Yb 2           ppm Condie 1993
Andesites 70 Yb 2.1           ppm Condie 1993
Andesites 70 Yb 1.8           ppm Condie 1993
Andesites 70 Yb 2           ppm Condie 1993
Andesites 40 Zr 150           ppm Condie 1993
Andesites 40 Zr 145           ppm Condie 1993
Andesites 40 Zr 160           ppm Condie 1993
Andesites 40 Zr 142           ppm Condie 1993
Andesites 40 Zr 160           ppm Condie 1993
Andesites 40 Zr 150           ppm Condie 1993
Andesites 40 Zr 153           ppm Condie 1993
Basalts 13 Al 15.7           wt%ox Condie 1993
Basalts 13 Al 15           wt%ox Condie 1993
Basalts 13 Al 15.3           wt%ox Condie 1993
Basalts 13 Al 15.3           wt%ox Condie 1993
Basalts 13 Al 15.5           wt%ox Condie 1993
Basalts 13 Al 15.7           wt%ox Condie 1993
Basalts 13 Al 15.8           wt%ox Condie 1993
Basalts 56 Ba 147           ppm Condie 1993
Basalts 56 Ba 204           ppm Condie 1993
Basalts 56 Ba 315           ppm Condie 1993
Basalts 56 Ba 277           ppm Condie 1993
Basalts 56 Ba 410           ppm Condie 1993
Basalts 56 Ba 380           ppm Condie 1993
Basalts 56 Ba 330           ppm Condie 1993
Basalts 20 Ca 10.2           wt%ox Condie 1993
Basalts 20 Ca 9.5           wt%ox Condie 1993
Basalts 20 Ca 9.5           wt%ox Condie 1993
Basalts 20 Ca 10           wt%ox Condie 1993
Basalts 20 Ca 9.6           wt%ox Condie 1993
Basalts 20 Ca 9.4           wt%ox Condie 1993
Basalts 20 Ca 9.5           wt%ox Condie 1993
Basalts 58 Ce 30           ppm Condie 1993
Basalts 58 Ce 15           ppm Condie 1993
Basalts 58 Ce 28           ppm Condie 1993
Basalts 58 Ce 31           ppm Condie 1993
Basalts 58 Ce 27           ppm Condie 1993
Basalts 58 Ce 27           ppm Condie 1993
Basalts 58 Ce 19           ppm Condie 1993
Basalts 27 Co 40           ppm Condie 1993
Basalts 27 Co 41           ppm Condie 1993
Basalts 27 Co 35           ppm Condie 1993
Basalts 27 Co 59           ppm Condie 1993
Basalts 27 Co 42           ppm Condie 1993
Basalts 27 Co 55           ppm Condie 1993
Basalts 27 Co 35           ppm Condie 1993
Basalts 24 Cr 158           ppm Condie 1993
Basalts 24 Cr 150           ppm Condie 1993
Basalts 24 Cr 456           ppm Condie 1993
Basalts 24 Cr 152           ppm Condie 1993
Basalts 24 Cr 406           ppm Condie 1993
Basalts 24 Cr 147           ppm Condie 1993
Basalts 24 Cr 182           ppm Condie 1993
Basalts 63 Eu 1           ppm Condie 1993
Basalts 63 Eu 1.3           ppm Condie 1993
Basalts 63 Eu 1.4           ppm Condie 1993
Basalts 63 Eu 1.2           ppm Condie 1993
Basalts 63 Eu 1           ppm Condie 1993
Basalts 63 Eu 1.3           ppm Condie 1993
Basalts 63 Eu 1.2           ppm Condie 1993
Basalts   Eu/Eu* 1.09             Condie 1993
Basalts   Eu/Eu* 1             Condie 1993
Basalts   Eu/Eu* 0.97             Condie 1993
Basalts   Eu/Eu* 1.07             Condie 1993
Basalts   Eu/Eu* 0.98             Condie 1993
Basalts   Eu/Eu* 0.84             Condie 1993
Basalts   Eu/Eu* 0.96             Condie 1993
Basalts 26 Fe 8.9           wt%ox Condie 1993
Basalts 26 Fe 10.8           wt%ox Condie 1993
Basalts 26 Fe 10.2           wt%ox Condie 1993
Basalts 26 Fe 9.5           wt%ox Condie 1993
Basalts 26 Fe 9.4           wt%ox Condie 1993
Basalts 26 Fe 9.1           wt%ox Condie 1993
Basalts 26 Fe 9           wt%ox Condie 1993
Basalts 64 Gd 4.52           ppm Interpolated from Sm and Tb. Condie 1993
Basalts 64 Gd 3.26           ppm Interpolated from Sm and Tb. Condie 1993
Basalts 64 Gd 4.03           ppm Interpolated from Sm and Tb. Condie 1993
Basalts 64 Gd 3.57           ppm Interpolated from Sm and Tb. Condie 1993
Basalts 64 Gd 4.01           ppm Interpolated from Sm and Tb. Condie 1993
Basalts 64 Gd 3.84           ppm Interpolated from Sm and Tb. Condie 1993
Basalts 64 Gd 4.22           ppm Interpolated from Sm and Tb. Condie 1993
Basalts 72 Hf 2.2           ppm Condie 1993
Basalts 72 Hf 3.3           ppm Condie 1993
Basalts 72 Hf 3.1           ppm Condie 1993
Basalts 72 Hf 3.5           ppm Condie 1993
Basalts 72 Hf 3.3           ppm Condie 1993
Basalts 72 Hf 2.6           ppm Condie 1993
Basalts 72 Hf 3.4           ppm Condie 1993
Basalts 19 K 0.33           wt%ox Condie 1993
Basalts 19 K 0.43           wt%ox Condie 1993
Basalts 19 K 0.83           wt%ox Condie 1993
Basalts 19 K 0.84           wt%ox Condie 1993
Basalts 19 K 0.85           wt%ox Condie 1993
Basalts 19 K 0.88           wt%ox Condie 1993
Basalts 19 K 0.76           wt%ox Condie 1993
Basalts 57 La 13           ppm Condie 1993
Basalts 57 La 7.5           ppm Condie 1993
Basalts 57 La 11           ppm Condie 1993
Basalts 57 La 11.3           ppm Condie 1993
Basalts 57 La 5.5           ppm Condie 1993
Basalts 57 La 11           ppm Condie 1993
Basalts 57 La 12           ppm Condie 1993
Basalts   La[n]/Yb[n] 2.8             Condie 1993
Basalts   La[n]/Yb[n] 2.5             Condie 1993
Basalts   La[n]/Yb[n] 2             Condie 1993
Basalts   La[n]/Yb[n] 2.8             Condie 1993
Basalts   La[n]/Yb[n] 1.3             Condie 1993
Basalts   La[n]/Yb[n] 2.7             Condie 1993
Basalts   La[n]/Yb[n] 2.5             Condie 1993
Basalts 71 Lu 0.45           ppm Condie 1993
Basalts 71 Lu 0.43           ppm Condie 1993
Basalts 71 Lu 0.38           ppm Condie 1993
Basalts 71 Lu 0.42           ppm Condie 1993
Basalts 71 Lu 0.4           ppm Condie 1993
Basalts 71 Lu 0.49           ppm Condie 1993
Basalts 71 Lu 0.45           ppm Condie 1993
Basalts 12 Mg 6.5           wt%ox Condie 1993
Basalts 12 Mg 7.6           wt%ox Condie 1993
Basalts 12 Mg 9.4           wt%ox Condie 1993
Basalts 12 Mg 6.9           wt%ox Condie 1993
Basalts 12 Mg 6.6           wt%ox Condie 1993
Basalts 12 Mg 6.7           wt%ox Condie 1993
Basalts 12 Mg 6           wt%ox Condie 1993
Basalts 11 Na 2.7           wt%ox Condie 1993
Basalts 11 Na 2.7           wt%ox Condie 1993
Basalts 11 Na 3.1           wt%ox Condie 1993
Basalts 11 Na 3           wt%ox Condie 1993
Basalts 11 Na 2.9           wt%ox Condie 1993
Basalts 11 Na 2.4           wt%ox Condie 1993
Basalts 11 Na 2.6           wt%ox Condie 1993
Basalts 41 Nb 5           ppm Condie 1993
Basalts 41 Nb 5           ppm Condie 1993
Basalts 41 Nb 4.5           ppm Condie 1993
Basalts 41 Nb 4           ppm Condie 1993
Basalts 41 Nb 4.5           ppm Condie 1993
Basalts 41 Nb 5           ppm Condie 1993
Basalts 41 Nb 5.5           ppm Condie 1993
Basalts 60 Nd 11           ppm Condie 1993
Basalts 60 Nd 9.6           ppm Condie 1993
Basalts 60 Nd 15           ppm Condie 1993
Basalts 60 Nd 15           ppm Condie 1993
Basalts 60 Nd 15           ppm Condie 1993
Basalts 60 Nd 16           ppm Condie 1993
Basalts 60 Nd 14           ppm Condie 1993
Basalts 28 Ni 83           ppm Condie 1993
Basalts 28 Ni 190           ppm Condie 1993
Basalts 28 Ni 68           ppm Condie 1993
Basalts 28 Ni 78           ppm Condie 1993
Basalts 28 Ni 96           ppm Condie 1993
Basalts 28 Ni 70           ppm Condie 1993
Basalts 28 Ni 182           ppm Condie 1993
Basalts 15 P 0.12           wt%ox Condie 1993
Basalts 15 P 0.11           wt%ox Condie 1993
Basalts 15 P 0.23           wt%ox Condie 1993
Basalts 15 P 0.24           wt%ox Condie 1993
Basalts 15 P 0.28           wt%ox Condie 1993
Basalts 15 P 0.26           wt%ox Condie 1993
Basalts 15 P 0.2           wt%ox Condie 1993
Basalts 82 Pb 5           ppm Condie 1993
Basalts 82 Pb 5           ppm Condie 1993
Basalts 82 Pb 6           ppm Condie 1993
Basalts 82 Pb 6           ppm Condie 1993
Basalts 82 Pb 6           ppm Condie 1993
Basalts 82 Pb 6           ppm Condie 1993
Basalts 82 Pb 6           ppm Condie 1993
Basalts 37 Rb 12           ppm Condie 1993
Basalts 37 Rb 9           ppm Condie 1993
Basalts 37 Rb 25           ppm Condie 1993
Basalts 37 Rb 23           ppm Condie 1993
Basalts 37 Rb 29           ppm Condie 1993
Basalts 37 Rb 23           ppm Condie 1993
Basalts 37 Rb 28           ppm Condie 1993
Basalts 21 Sc 35           ppm Condie 1993
Basalts 21 Sc 37           ppm Condie 1993
Basalts 21 Sc 40           ppm Condie 1993
Basalts 21 Sc 33           ppm Condie 1993
Basalts 21 Sc 35           ppm Condie 1993
Basalts 21 Sc 37           ppm Condie 1993
Basalts 21 Sc 33           ppm Condie 1993
Basalts 14 Si 50.5           wt%ox Condie 1993
Basalts 14 Si 50.5           wt%ox Condie 1993
Basalts 14 Si 50.3           wt%ox Condie 1993
Basalts 14 Si 50.8           wt%ox Condie 1993
Basalts 14 Si 50.3           wt%ox Condie 1993
Basalts 14 Si 50.2           wt%ox Condie 1993
Basalts 14 Si 50.7           wt%ox Condie 1993
Basalts 62 Sm 3.8           ppm Condie 1993
Basalts 62 Sm 4           ppm Condie 1993
Basalts 62 Sm 2.8           ppm Condie 1993
Basalts 62 Sm 3.5           ppm Condie 1993
Basalts 62 Sm 3.7           ppm Condie 1993
Basalts 62 Sm 3           ppm Condie 1993
Basalts 62 Sm 4.3           ppm Condie 1993
Basalts 38 Sr 132           ppm Condie 1993
Basalts 38 Sr 240           ppm Condie 1993
Basalts 38 Sr 280           ppm Condie 1993
Basalts 38 Sr 222           ppm Condie 1993
Basalts 38 Sr 236           ppm Condie 1993
Basalts 38 Sr 260           ppm Condie 1993
Basalts 38 Sr 150           ppm Condie 1993
Basalts 73 Ta 0.23           ppm Condie 1993
Basalts 73 Ta 0.27           ppm Condie 1993
Basalts 73 Ta 0.3           ppm Condie 1993
Basalts 73 Ta 0.25           ppm Condie 1993
Basalts 73 Ta 0.3           ppm Condie 1993
Basalts 73 Ta 0.25           ppm Condie 1993
Basalts 73 Ta 0.24           ppm Condie 1993
Basalts 65 Tb 0.68           ppm Condie 1993
Basalts 65 Tb 0.65           ppm Condie 1993
Basalts 65 Tb 0.65           ppm Condie 1993
Basalts 65 Tb 0.72           ppm Condie 1993
Basalts 65 Tb 0.75           ppm Condie 1993
Basalts 65 Tb 0.65           ppm Condie 1993
Basalts 65 Tb 0.55           ppm Condie 1993
Basalts 90 Th 2.4           ppm Condie 1993
Basalts 90 Th 2.6           ppm Condie 1993
Basalts 90 Th 2.6           ppm Condie 1993
Basalts 90 Th 1           ppm Condie 1993
Basalts 90 Th 1           ppm Condie 1993
Basalts 90 Th 2.4           ppm Condie 1993
Basalts 90 Th 2.4           ppm Condie 1993
Basalts 22 Ti 1.5           wt%ox Condie 1993
Basalts 22 Ti 1.45           wt%ox Condie 1993
Basalts 22 Ti 0.99           wt%ox Condie 1993
Basalts 22 Ti 0.97           wt%ox Condie 1993
Basalts 22 Ti 1.42           wt%ox Condie 1993
Basalts 22 Ti 1.52           wt%ox Condie 1993
Basalts 22 Ti 1.45           wt%ox Condie 1993
Basalts 92 U 1           ppm Condie 1993
Basalts 92 U 1.5           ppm Condie 1993
Basalts 92 U 1.2           ppm Condie 1993
Basalts 92 U 1.2           ppm Condie 1993
Basalts 92 U 1           ppm Condie 1993
Basalts 92 U 1.3           ppm Condie 1993
Basalts 92 U 1.2           ppm Condie 1993
Basalts 23 V 272           ppm Condie 1993
Basalts 23 V 240           ppm Condie 1993
Basalts 23 V 260           ppm Condie 1993
Basalts 23 V 283           ppm Condie 1993
Basalts 23 V 252           ppm Condie 1993
Basalts 23 V 270           ppm Condie 1993
Basalts 23 V 245           ppm Condie 1993
Basalts 39 Y 20           ppm Condie 1993
Basalts 39 Y 33           ppm Condie 1993
Basalts 39 Y 28           ppm Condie 1993
Basalts 39 Y 27           ppm Condie 1993
Basalts 39 Y 30           ppm Condie 1993
Basalts 39 Y 23           ppm Condie 1993
Basalts 39 Y 32           ppm Condie 1993
Basalts 70 Yb 2.8           ppm Condie 1993
Basalts 70 Yb 2.3           ppm Condie 1993
Basalts 70 Yb 2.6           ppm Condie 1993
Basalts 70 Yb 2.5           ppm Condie 1993
Basalts 70 Yb 2.5           ppm Condie 1993
Basalts 70 Yb 2.7           ppm Condie 1993
Basalts 70 Yb 2.7           ppm Condie 1993
Basalts 40 Zr 82           ppm Condie 1993
Basalts 40 Zr 130           ppm Condie 1993
Basalts 40 Zr 128           ppm Condie 1993
Basalts 40 Zr 133           ppm Condie 1993
Basalts 40 Zr 138           ppm Condie 1993
Basalts 40 Zr 98           ppm Condie 1993
Basalts 40 Zr 131           ppm Condie 1993
Early Archean Upper Crust 13 Al 14.65           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust 13 Al 14.57           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust   Al2O3/SiO2 0.22             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust   Al2O3/SiO2 0.22             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust   Al2O3/TiO2 35             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust   Al2O3/TiO2 32             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust 56 Ba 561           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust 56 Ba 526           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust   Ba/La 18             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust   Ba/La 19             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust   Ba/Nb 62             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust   Ba/Nb 69             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust   Ba/Rb 7.4             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust   Ba/Rb 7.8             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust   Ba/Sr 2             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust   Ba/Sr 2.1             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust 20 Ca 3.51           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. CaO is that remaining after apatite is subtracted assuming all P2O5 is residing in apatite. Condie 1993
Early Archean Upper Crust 20 Ca 3.81           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. CaO is that remaining after apatite is subtracted assuming all P2O5 is residing in apatite. Condie 1993
Early Archean Upper Crust 58 Ce 56.5           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust 58 Ce 55.3           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust   CIW 54.4             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust   CIW 54.9             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust 27 Co 25           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust 27 Co 22           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust   Co/Th 3.4             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust   Co/Th 2.8             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust 24 Cr 286           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust 24 Cr 231           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust   Cr/Ni 1.7             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust   Cr/Ni 1.7             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust   Cr/Sc 22             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust   Cr/Sc 21             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust   Cr/Th 38             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust   Cr/Th 30             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust   Cr/V 3.5             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust   Cr/V 3.3             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust 63 Eu 0.97           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust 63 Eu 0.97           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust   Eu/Eu* 0.78             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust   Eu/Eu* 0.81             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust 26 Fe 4.92           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust 26 Fe 4.53           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust 64 Gd 3.58           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Interpolated from Sm and Tb. Condie 1993
Early Archean Upper Crust 64 Gd 3.47           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Interpolated from Sm and Tb. Condie 1993
Early Archean Upper Crust 72 Hf 3.7           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust 72 Hf 3.8           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust 19 K 2.52           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust 19 K 2.46           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust   K/Rb 288             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust   K/Rb 291             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust   K2O/Na2O 0.73             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust   K2O/Na2O 0.7             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust 57 La 28.5           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust 57 La 29.4           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust   La/Sc 2.2             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust   La/Sc 2.7             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust   La/Ta 42             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust   La/Ta 41             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust   La/Th 3.8             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust   La/Th 3.8             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust   La[n]/Yb[n] 12             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust   La[n]/Yb[n] 10.6             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust 71 Lu 0.27           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust 71 Lu 0.25           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust   Lu/Hf 0.072             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust   Lu/Hf 0.066             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust 12 Mg 4.06           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust 12 Mg 3.4           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust 11 Na 3.59           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust 11 Na 3.36           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust 41 Nb 8.4           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust 41 Nb 8.5           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust   Nb/Ta 12             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust   Nb/Ta 12             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust 60 Nd 24.9           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust 60 Nd 25           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust 28 Ni 164           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust 28 Ni 134           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust   Ni/Co 6.4             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust   Ni/Co 6.1             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust 15 P 0.1           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust 15 P 0.1           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust 82 Pb 17           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust 82 Pb 18           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust 37 Rb 71           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust 37 Rb 72           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust   Rb/Sr 0.28             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust   Rb/Sr 0.25             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust 21 Sc 11           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust 21 Sc 13.1           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust 14 Si 66.42           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust 14 Si 65.35           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust 62 Sm 3.96           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust 62 Sm 4.05           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust   Sm/Nd 0.159             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust   Sm/Nd 0.162             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust 38 Sr 287           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust 38 Sr 251           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust 73 Ta 0.7           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust 73 Ta 0.69           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust 65 Tb 0.55           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust 65 Tb 0.53           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust 90 Th 7.5           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust 90 Th 7.8           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust   Th/Nb 0.93             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust   Th/Nb 0.88             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust   Th/Sc 0.71             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust   Th/Sc 0.57             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust   Th/U 3.9             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust   Th/U 3.9             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust 22 Ti 0.42           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust 22 Ti 0.46           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust   Ti/Zr 17             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust   Ti/Zr 20             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust 92 U 2           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust 92 U 1.9           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust 23 V 70           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust 23 V 81           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust 39 Y 17           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust 39 Y 18           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust 70 Yb 1.63           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust 70 Yb 1.49           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust 40 Zr 145           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust 40 Zr 140           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Archean Upper Crust   Zr/Hf 38             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust   Zr/Hf 38             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust   Zr/Nb 16             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust   Zr/Nb 17             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust   Zr/Y 7.7             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Archean Upper Crust   Zr/Y 8.5             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust 13 Al 14.9           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust 13 Al 15.01           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust   Al2O3/SiO2 0.23             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust   Al2O3/SiO2 0.22             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust   Al2O3/TiO2 26             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust   Al2O3/TiO2 24             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust 56 Ba 684           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust 56 Ba 700           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust   Ba/La 24             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust   Ba/La 23             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust   Ba/Nb 58             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust   Ba/Nb 61             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust   Ba/Rb 7             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust   Ba/Rb 7.4             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust   Ba/Sr 2.5             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust   Ba/Sr 2.4             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust 20 Ca 3.52           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. CaO is that remaining after apatite is subtracted assuming all P2O5 is residing in apatite. Condie 1993
Early Proterozoic Upper Crust 20 Ca 3.2           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. CaO is that remaining after apatite is subtracted assuming all P2O5 is residing in apatite. Condie 1993
Early Proterozoic Upper Crust 58 Ce 65.3           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust 58 Ce 59.6           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust   CIW 56.7             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust   CIW 57.6             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust 27 Co 17           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust 27 Co 15           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust   Co/Th 1.5             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust   Co/Th 1.9             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust 24 Cr 68           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust 24 Cr 59           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust   Cr/Ni 1.9             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust   Cr/Ni 1.9             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust   Cr/Sc 4.1             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust   Cr/Sc 4.2             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust   Cr/Th 5.7             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust   Cr/Th 7.4             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust   Cr/V 0.75             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust   Cr/V 0.74             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust 63 Eu 1.21           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust 63 Eu 1.19           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust   Eu/Eu* 0.73             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust   Eu/Eu* 0.68             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust 26 Fe 4.83           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust 26 Fe 4.46           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust 64 Gd 4.92           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Interpolated from Sm and Tb. Condie 1993
Early Proterozoic Upper Crust 64 Gd 5.24           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Interpolated from Sm and Tb. Condie 1993
Early Proterozoic Upper Crust 72 Hf 4.9           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust 72 Hf 5.1           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust 19 K 3.22           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust 19 K 2.97           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust   K/Rb 269             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust   K/Rb 268             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust   K2O/Na2O 0.9             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust   K2O/Na2O 0.97             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust 57 La 30.9           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust 57 La 28.8           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust   La/Sc 1.8             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust   La/Sc 2.1             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust   La/Ta 33             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust   La/Ta 33             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust   La/Th 3.1             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust   La/Th 3             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust   La[n]/Yb[n] 8.1             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust   La[n]/Yb[n] 7.8             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust 71 Lu 0.38           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust 71 Lu 0.36           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust   Lu/Hf 0.074             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust   Lu/Hf 0.075             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust 12 Mg 2.23           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust 12 Mg 1.95           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust 11 Na 3.31           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust 11 Na 3.29           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust 41 Nb 12.1           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust 41 Nb 11.2           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust   Nb/Ta 13             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust   Nb/Ta 13             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust 60 Nd 29.8           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust 60 Nd 27           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust 28 Ni 31           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust 28 Ni 36           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust   Ni/Co 2.1             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust   Ni/Co 2             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust 15 P 0.13           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust 15 P 0.14           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust 82 Pb 17           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust 82 Pb 18           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust 37 Rb 99           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust 37 Rb 92           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust   Rb/Sr 0.32             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust   Rb/Sr 0.36             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust 21 Sc 14.5           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust 21 Sc 16.3           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust 14 Si 66.86           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust 14 Si 65.86           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust 62 Sm 5.59           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust 62 Sm 5.22           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust   Sm/Nd 0.188             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust   Sm/Nd 0.193             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust 38 Sr 280           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust 38 Sr 287           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust 73 Ta 0.88           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust 73 Ta 0.95           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust 65 Tb 0.77           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust 65 Tb 0.82           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust 90 Th 9.2           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust 90 Th 10.4           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust   Th/Nb 0.86             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust   Th/Nb 0.82             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust   Th/Sc 0.56             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust   Th/Sc 0.72             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust   Th/U 3.9             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust   Th/U 4             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust 22 Ti 0.58           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust 22 Ti 0.63           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust   Ti/Zr 22             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust   Ti/Zr 19             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust 92 U 2.6           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust 92 U 2.4           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust 23 V 81           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust 23 V 91           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust 39 Y 32           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust 39 Y 30           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust 70 Yb 2.23           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust 70 Yb 2.32           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust 40 Zr 180           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust 40 Zr 174           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Early Proterozoic Upper Crust   Zr/Hf 35             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust   Zr/Hf 36             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust   Zr/Nb 16             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust   Zr/Nb 15             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust   Zr/Y 5.7             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Early Proterozoic Upper Crust   Zr/Y 5.7             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Felsic Volcanics 13 Al 13.4           wt%ox Condie 1993
Felsic Volcanics 13 Al 13.8           wt%ox Condie 1993
Felsic Volcanics 13 Al 14           wt%ox Condie 1993
Felsic Volcanics 13 Al 14.2           wt%ox Condie 1993
Felsic Volcanics 13 Al 13.2           wt%ox Condie 1993
Felsic Volcanics 13 Al 14.3           wt%ox Condie 1993
Felsic Volcanics 13 Al 13.9           wt%ox Condie 1993
Felsic Volcanics 56 Ba 850           ppm Condie 1993
Felsic Volcanics 56 Ba 900           ppm Condie 1993
Felsic Volcanics 56 Ba 850           ppm Condie 1993
Felsic Volcanics 56 Ba 360           ppm Condie 1993
Felsic Volcanics 56 Ba 952           ppm Condie 1993
Felsic Volcanics 56 Ba 480           ppm Condie 1993
Felsic Volcanics 56 Ba 900           ppm Condie 1993
Felsic Volcanics 20 Ca 1.6           wt%ox Condie 1993
Felsic Volcanics 20 Ca 1.2           wt%ox Condie 1993
Felsic Volcanics 20 Ca 1.25           wt%ox Condie 1993
Felsic Volcanics 20 Ca 1.2           wt%ox Condie 1993
Felsic Volcanics 20 Ca 1.4           wt%ox Condie 1993
Felsic Volcanics 20 Ca 1.3           wt%ox Condie 1993
Felsic Volcanics 20 Ca 1.5           wt%ox Condie 1993
Felsic Volcanics 58 Ce 51.2           ppm Condie 1993
Felsic Volcanics 58 Ce 65           ppm Condie 1993
Felsic Volcanics 58 Ce 71           ppm Condie 1993
Felsic Volcanics 58 Ce 45           ppm Condie 1993
Felsic Volcanics 58 Ce 48           ppm Condie 1993
Felsic Volcanics 58 Ce 59           ppm Condie 1993
Felsic Volcanics 58 Ce 69           ppm Condie 1993
Felsic Volcanics 27 Co 5           ppm Condie 1993
Felsic Volcanics 27 Co 6           ppm Condie 1993
Felsic Volcanics 27 Co 5           ppm Condie 1993
Felsic Volcanics 27 Co 6           ppm Condie 1993
Felsic Volcanics 27 Co 12           ppm Condie 1993
Felsic Volcanics 27 Co 6           ppm Condie 1993
Felsic Volcanics 27 Co 10           ppm Condie 1993
Felsic Volcanics 24 Cr 5           ppm Condie 1993
Felsic Volcanics 24 Cr 6           ppm Condie 1993
Felsic Volcanics 24 Cr 7           ppm Condie 1993
Felsic Volcanics 24 Cr 9           ppm Condie 1993
Felsic Volcanics 24 Cr 25           ppm Condie 1993
Felsic Volcanics 24 Cr 20           ppm Condie 1993
Felsic Volcanics 24 Cr 10           ppm Condie 1993
Felsic Volcanics 63 Eu 1           ppm Condie 1993
Felsic Volcanics 63 Eu 1.5           ppm Condie 1993
Felsic Volcanics 63 Eu 1.1           ppm Condie 1993
Felsic Volcanics 63 Eu 1.2           ppm Condie 1993
Felsic Volcanics 63 Eu 0.8           ppm Condie 1993
Felsic Volcanics 63 Eu 0.9           ppm Condie 1993
Felsic Volcanics 63 Eu 1.5           ppm Condie 1993
Felsic Volcanics   Eu/Eu* 0.87             Condie 1993
Felsic Volcanics   Eu/Eu* 0.82             Condie 1993
Felsic Volcanics   Eu/Eu* 0.85             Condie 1993
Felsic Volcanics   Eu/Eu* 0.66             Condie 1993
Felsic Volcanics   Eu/Eu* 0.82             Condie 1993
Felsic Volcanics   Eu/Eu* 0.56             Condie 1993
Felsic Volcanics   Eu/Eu* 0.48             Condie 1993
Felsic Volcanics 26 Fe 2.8           wt%ox Condie 1993
Felsic Volcanics 26 Fe 2.7           wt%ox Condie 1993
Felsic Volcanics 26 Fe 2.5           wt%ox Condie 1993
Felsic Volcanics 26 Fe 3.2           wt%ox Condie 1993
Felsic Volcanics 26 Fe 2.7           wt%ox Condie 1993
Felsic Volcanics 26 Fe 3.5           wt%ox Condie 1993
Felsic Volcanics 26 Fe 2.8           wt%ox Condie 1993
Felsic Volcanics 64 Gd 4.72           ppm Interpolated from Sm and Tb. Condie 1993
Felsic Volcanics 64 Gd 4.37           ppm Interpolated from Sm and Tb. Condie 1993
Felsic Volcanics 64 Gd 4.87           ppm Interpolated from Sm and Tb. Condie 1993
Felsic Volcanics 64 Gd 5.8           ppm Interpolated from Sm and Tb. Condie 1993
Felsic Volcanics 64 Gd 4.72           ppm Interpolated from Sm and Tb. Condie 1993
Felsic Volcanics 64 Gd 5.72           ppm Interpolated from Sm and Tb. Condie 1993
Felsic Volcanics 64 Gd 4.26           ppm Interpolated from Sm and Tb. Condie 1993
Felsic Volcanics 72 Hf 5.5           ppm Condie 1993
Felsic Volcanics 72 Hf 5.7           ppm Condie 1993
Felsic Volcanics 72 Hf 6.5           ppm Condie 1993
Felsic Volcanics 72 Hf 5.1           ppm Condie 1993
Felsic Volcanics 72 Hf 6.5           ppm Condie 1993
Felsic Volcanics 72 Hf 6           ppm Condie 1993
Felsic Volcanics 72 Hf 6.5           ppm Condie 1993
Felsic Volcanics 19 K 4.3           wt%ox Condie 1993
Felsic Volcanics 19 K 4.1           wt%ox Condie 1993
Felsic Volcanics 19 K 4.1           wt%ox Condie 1993
Felsic Volcanics 19 K 3.7           wt%ox Condie 1993
Felsic Volcanics 19 K 4           wt%ox Condie 1993
Felsic Volcanics 19 K 2.3           wt%ox Condie 1993
Felsic Volcanics 19 K 2.1           wt%ox Condie 1993
Felsic Volcanics 57 La 35           ppm Condie 1993
Felsic Volcanics 57 La 28           ppm Condie 1993
Felsic Volcanics 57 La 20           ppm Condie 1993
Felsic Volcanics 57 La 20           ppm Condie 1993
Felsic Volcanics 57 La 30           ppm Condie 1993
Felsic Volcanics 57 La 25           ppm Condie 1993
Felsic Volcanics 57 La 28           ppm Condie 1993
Felsic Volcanics   La[n]/Yb[n] 3.1             Condie 1993
Felsic Volcanics   La[n]/Yb[n] 6.3             Condie 1993
Felsic Volcanics   La[n]/Yb[n] 6.1             Condie 1993
Felsic Volcanics   La[n]/Yb[n] 5.9             Condie 1993
Felsic Volcanics   La[n]/Yb[n] 3.1             Condie 1993
Felsic Volcanics   La[n]/Yb[n] 5.8             Condie 1993
Felsic Volcanics   La[n]/Yb[n] 6.8             Condie 1993
Felsic Volcanics 71 Lu 0.48           ppm Condie 1993
Felsic Volcanics 71 Lu 0.78           ppm Condie 1993
Felsic Volcanics 71 Lu 0.48           ppm Condie 1993
Felsic Volcanics 71 Lu 0.5           ppm Condie 1993
Felsic Volcanics 71 Lu 0.6           ppm Condie 1993
Felsic Volcanics 71 Lu 0.4           ppm Condie 1993
Felsic Volcanics 71 Lu 0.6           ppm Condie 1993
Felsic Volcanics 12 Mg 0.4           wt%ox Condie 1993
Felsic Volcanics 12 Mg 0.6           wt%ox Condie 1993
Felsic Volcanics 12 Mg 0.5           wt%ox Condie 1993
Felsic Volcanics 12 Mg 0.81           wt%ox Condie 1993
Felsic Volcanics 12 Mg 0.5           wt%ox Condie 1993
Felsic Volcanics 12 Mg 0.99           wt%ox Condie 1993
Felsic Volcanics 12 Mg 0.74           wt%ox Condie 1993
Felsic Volcanics 11 Na 3.5           wt%ox Condie 1993
Felsic Volcanics 11 Na 4.5           wt%ox Condie 1993
Felsic Volcanics 11 Na 3.2           wt%ox Condie 1993
Felsic Volcanics 11 Na 3.7           wt%ox Condie 1993
Felsic Volcanics 11 Na 4.3           wt%ox Condie 1993
Felsic Volcanics 11 Na 3.3           wt%ox Condie 1993
Felsic Volcanics 11 Na 3.5           wt%ox Condie 1993
Felsic Volcanics 41 Nb 20           ppm Condie 1993
Felsic Volcanics 41 Nb 18           ppm Condie 1993
Felsic Volcanics 41 Nb 10           ppm Condie 1993
Felsic Volcanics 41 Nb 13           ppm Condie 1993
Felsic Volcanics 41 Nb 15           ppm Condie 1993
Felsic Volcanics 41 Nb 16           ppm Condie 1993
Felsic Volcanics 41 Nb 21           ppm Condie 1993
Felsic Volcanics 60 Nd 19           ppm Condie 1993
Felsic Volcanics 60 Nd 25           ppm Condie 1993
Felsic Volcanics 60 Nd 23           ppm Condie 1993
Felsic Volcanics 60 Nd 30.6           ppm Condie 1993
Felsic Volcanics 60 Nd 22           ppm Condie 1993
Felsic Volcanics 60 Nd 22           ppm Condie 1993
Felsic Volcanics 60 Nd 28           ppm Condie 1993
Felsic Volcanics 28 Ni 8           ppm Condie 1993
Felsic Volcanics 28 Ni 6           ppm Condie 1993
Felsic Volcanics 28 Ni 8           ppm Condie 1993
Felsic Volcanics 28 Ni 7           ppm Condie 1993
Felsic Volcanics 28 Ni 18           ppm Condie 1993
Felsic Volcanics 28 Ni 1.5           ppm Condie 1993
Felsic Volcanics 28 Ni 6           ppm Condie 1993
Felsic Volcanics 15 P 0.06           wt%ox Condie 1993
Felsic Volcanics 15 P 0.06           wt%ox Condie 1993
Felsic Volcanics 15 P 0.05           wt%ox Condie 1993
Felsic Volcanics 15 P 0.1           wt%ox Condie 1993
Felsic Volcanics 15 P 0.08           wt%ox Condie 1993
Felsic Volcanics 15 P 0.09           wt%ox Condie 1993
Felsic Volcanics 15 P 0.1           wt%ox Condie 1993
Felsic Volcanics 82 Pb 23           ppm Condie 1993
Felsic Volcanics 82 Pb 23           ppm Condie 1993
Felsic Volcanics 82 Pb 23           ppm Condie 1993
Felsic Volcanics 82 Pb 20           ppm Condie 1993
Felsic Volcanics 82 Pb 23           ppm Condie 1993
Felsic Volcanics 82 Pb 20           ppm Condie 1993
Felsic Volcanics 82 Pb 23           ppm Condie 1993
Felsic Volcanics 37 Rb 130           ppm Condie 1993
Felsic Volcanics 37 Rb 150           ppm Condie 1993
Felsic Volcanics 37 Rb 125           ppm Condie 1993
Felsic Volcanics 37 Rb 57           ppm Condie 1993
Felsic Volcanics 37 Rb 125           ppm Condie 1993
Felsic Volcanics 37 Rb 35           ppm Condie 1993
Felsic Volcanics 37 Rb 130           ppm Condie 1993
Felsic Volcanics 21 Sc 10           ppm Condie 1993
Felsic Volcanics 21 Sc 16           ppm Condie 1993
Felsic Volcanics 21 Sc 17           ppm Condie 1993
Felsic Volcanics 21 Sc 15           ppm Condie 1993
Felsic Volcanics 21 Sc 16           ppm Condie 1993
Felsic Volcanics 21 Sc 13           ppm Condie 1993
Felsic Volcanics 21 Sc 16           ppm Condie 1993
Felsic Volcanics 14 Si 73           wt%ox Condie 1993
Felsic Volcanics 14 Si 72.2           wt%ox Condie 1993
Felsic Volcanics 14 Si 73.3           wt%ox Condie 1993
Felsic Volcanics 14 Si 73           wt%ox Condie 1993
Felsic Volcanics 14 Si 73.6           wt%ox Condie 1993
Felsic Volcanics 14 Si 73.6           wt%ox Condie 1993
Felsic Volcanics 14 Si 73.2           wt%ox Condie 1993
Felsic Volcanics 62 Sm 5.6           ppm Condie 1993
Felsic Volcanics 62 Sm 5           ppm Condie 1993
Felsic Volcanics 62 Sm 5           ppm Condie 1993
Felsic Volcanics 62 Sm 4           ppm Condie 1993
Felsic Volcanics 62 Sm 4.3           ppm Condie 1993
Felsic Volcanics 62 Sm 4.9           ppm Condie 1993
Felsic Volcanics 62 Sm 5.1           ppm Condie 1993
Felsic Volcanics 38 Sr 160           ppm Condie 1993
Felsic Volcanics 38 Sr 170           ppm Condie 1993
Felsic Volcanics 38 Sr 150           ppm Condie 1993
Felsic Volcanics 38 Sr 136           ppm Condie 1993
Felsic Volcanics 38 Sr 150           ppm Condie 1993
Felsic Volcanics 38 Sr 111           ppm Condie 1993
Felsic Volcanics 38 Sr 125           ppm Condie 1993
Felsic Volcanics 73 Ta 1.7           ppm Condie 1993
Felsic Volcanics 73 Ta 1.3           ppm Condie 1993
Felsic Volcanics 73 Ta 1.2           ppm Condie 1993
Felsic Volcanics 73 Ta 0.8           ppm Condie 1993
Felsic Volcanics 73 Ta 1.6           ppm Condie 1993
Felsic Volcanics 73 Ta 1.4           ppm Condie 1993
Felsic Volcanics 73 Ta 1           ppm Condie 1993
Felsic Volcanics 65 Tb 0.71           ppm Condie 1993
Felsic Volcanics 65 Tb 0.78           ppm Condie 1993
Felsic Volcanics 65 Tb 0.66           ppm Condie 1993
Felsic Volcanics 65 Tb 1           ppm Condie 1993
Felsic Volcanics 65 Tb 0.7           ppm Condie 1993
Felsic Volcanics 65 Tb 1           ppm Condie 1993
Felsic Volcanics 65 Tb 0.8           ppm Condie 1993
Felsic Volcanics 90 Th 8.5           ppm Condie 1993
Felsic Volcanics 90 Th 9           ppm Condie 1993
Felsic Volcanics 90 Th 8.2           ppm Condie 1993
Felsic Volcanics 90 Th 10.2           ppm Condie 1993
Felsic Volcanics 90 Th 8           ppm Condie 1993
Felsic Volcanics 90 Th 2           ppm Condie 1993
Felsic Volcanics 90 Th 2           ppm Condie 1993
Felsic Volcanics 22 Ti 0.35           wt%ox Condie 1993
Felsic Volcanics 22 Ti 0.35           wt%ox Condie 1993
Felsic Volcanics 22 Ti 0.29           wt%ox Condie 1993
Felsic Volcanics 22 Ti 0.34           wt%ox Condie 1993
Felsic Volcanics 22 Ti 0.25           wt%ox Condie 1993
Felsic Volcanics 22 Ti 0.25           wt%ox Condie 1993
Felsic Volcanics 22 Ti 0.28           wt%ox Condie 1993
Felsic Volcanics 92 U 2.5           ppm Condie 1993
Felsic Volcanics 92 U 2.3           ppm Condie 1993
Felsic Volcanics 92 U 2.5           ppm Condie 1993
Felsic Volcanics 92 U 2.3           ppm Condie 1993
Felsic Volcanics 92 U 2.5           ppm Condie 1993
Felsic Volcanics 92 U 0.6           ppm Condie 1993
Felsic Volcanics 92 U 0.6           ppm Condie 1993
Felsic Volcanics 23 V 30           ppm Condie 1993
Felsic Volcanics 23 V 25           ppm Condie 1993
Felsic Volcanics 23 V 30           ppm Condie 1993
Felsic Volcanics 23 V 48           ppm Condie 1993
Felsic Volcanics 23 V 50           ppm Condie 1993
Felsic Volcanics 23 V 30           ppm Condie 1993
Felsic Volcanics 23 V 40           ppm Condie 1993
Felsic Volcanics 39 Y 37           ppm Condie 1993
Felsic Volcanics 39 Y 33           ppm Condie 1993
Felsic Volcanics 39 Y 38           ppm Condie 1993
Felsic Volcanics 39 Y 38           ppm Condie 1993
Felsic Volcanics 39 Y 35           ppm Condie 1993
Felsic Volcanics 39 Y 45           ppm Condie 1993
Felsic Volcanics 39 Y 40           ppm Condie 1993
Felsic Volcanics 70 Yb 3.1           ppm Condie 1993
Felsic Volcanics 70 Yb 2.76           ppm Condie 1993
Felsic Volcanics 70 Yb 2.9           ppm Condie 1993
Felsic Volcanics 70 Yb 3.9           ppm Condie 1993
Felsic Volcanics 70 Yb 2.9           ppm Condie 1993
Felsic Volcanics 70 Yb 3.9           ppm Condie 1993
Felsic Volcanics 70 Yb 2.6           ppm Condie 1993
Felsic Volcanics 40 Zr 215           ppm Condie 1993
Felsic Volcanics 40 Zr 215           ppm Condie 1993
Felsic Volcanics 40 Zr 230           ppm Condie 1993
Felsic Volcanics 40 Zr 215           ppm Condie 1993
Felsic Volcanics 40 Zr 230           ppm Condie 1993
Felsic Volcanics 40 Zr 215           ppm Condie 1993
Felsic Volcanics 40 Zr 230           ppm Condie 1993
Granites 13 Al 14.8           wt%ox Condie 1993
Granites 13 Al 13.4           wt%ox Condie 1993
Granites 13 Al 13.5           wt%ox Condie 1993
Granites 56 Ba 750           ppm Condie 1993
Granites 56 Ba 765           ppm Condie 1993
Granites 56 Ba 800           ppm Condie 1993
Granites 20 Ca 1.2           wt%ox Condie 1993
Granites 20 Ca 1.18           wt%ox Condie 1993
Granites 20 Ca 1.3           wt%ox Condie 1993
Granites 58 Ce 95           ppm Condie 1993
Granites 58 Ce 94           ppm Condie 1993
Granites 58 Ce 115           ppm Condie 1993
Granites 27 Co 5.5           ppm Condie 1993
Granites 27 Co 3           ppm Condie 1993
Granites 27 Co 3.5           ppm Condie 1993
Granites 24 Cr 16           ppm Condie 1993
Granites 24 Cr 18           ppm Condie 1993
Granites 24 Cr 8           ppm Condie 1993
Granites 63 Eu 0.85           ppm Condie 1993
Granites 63 Eu 0.9           ppm Condie 1993
Granites 63 Eu 1           ppm Condie 1993
Granites   Eu/Eu* 0.34             Condie 1993
Granites   Eu/Eu* 0.37             Condie 1993
Granites   Eu/Eu* 0.48             Condie 1993
Granites 26 Fe 1.94           wt%ox Condie 1993
Granites 26 Fe 2.2           wt%ox Condie 1993
Granites 26 Fe 2.3           wt%ox Condie 1993
Granites 64 Gd 4.67           ppm Interpolated from Sm and Tb. Condie 1993
Granites 64 Gd 8.17           ppm Interpolated from Sm and Tb. Condie 1993
Granites 64 Gd 7.63           ppm Interpolated from Sm and Tb. Condie 1993
Granites 72 Hf 4.5           ppm Condie 1993
Granites 72 Hf 7           ppm Condie 1993
Granites 72 Hf 6.5           ppm Condie 1993
Granites 19 K 4.8           wt%ox Condie 1993
Granites 19 K 4.8           wt%ox Condie 1993
Granites 19 K 4.94           wt%ox Condie 1993
Granites 57 La 50           ppm Condie 1993
Granites 57 La 48           ppm Condie 1993
Granites 57 La 40           ppm Condie 1993
Granites   La[n]/Yb[n] 15.2             Condie 1993
Granites   La[n]/Yb[n] 8.3             Condie 1993
Granites   La[n]/Yb[n] 7.6             Condie 1993
Granites 71 Lu 0.58           ppm Condie 1993
Granites 71 Lu 0.32           ppm Condie 1993
Granites 71 Lu 0.54           ppm Condie 1993
Granites 12 Mg 0.42           wt%ox Condie 1993
Granites 12 Mg 0.37           wt%ox Condie 1993
Granites 12 Mg 0.4           wt%ox Condie 1993
Granites 11 Na 3.5           wt%ox Condie 1993
Granites 11 Na 3.2           wt%ox Condie 1993
Granites 11 Na 3.16           wt%ox Condie 1993
Granites 41 Nb 12           ppm Condie 1993
Granites 41 Nb 20           ppm Condie 1993
Granites 41 Nb 21           ppm Condie 1993
Granites 60 Nd 46           ppm Condie 1993
Granites 60 Nd 46           ppm Condie 1993
Granites 60 Nd 54           ppm Condie 1993
Granites 28 Ni 15           ppm Condie 1993
Granites 28 Ni 12           ppm Condie 1993
Granites 28 Ni 7           ppm Condie 1993
Granites 15 P 0.08           wt%ox Condie 1993
Granites 15 P 0.09           wt%ox Condie 1993
Granites 15 P 0.08           wt%ox Condie 1993
Granites 82 Pb 25           ppm Condie 1993
Granites 82 Pb 25           ppm Condie 1993
Granites 82 Pb 25           ppm Condie 1993
Granites 37 Rb 156           ppm Condie 1993
Granites 37 Rb 150           ppm Condie 1993
Granites 37 Rb 170           ppm Condie 1993
Granites 21 Sc 5           ppm Condie 1993
Granites 21 Sc 4           ppm Condie 1993
Granites 21 Sc 5           ppm Condie 1993
Granites 14 Si 72.4           wt%ox Condie 1993
Granites 14 Si 73.3           wt%ox Condie 1993
Granites 14 Si 73.8           wt%ox Condie 1993
Granites 62 Sm 6.3           ppm Condie 1993
Granites 62 Sm 8.8           ppm Condie 1993
Granites 62 Sm 8.7           ppm Condie 1993
Granites 38 Sr 120           ppm Condie 1993
Granites 38 Sr 122           ppm Condie 1993
Granites 38 Sr 145           ppm Condie 1993
Granites 73 Ta 1           ppm Condie 1993
Granites 73 Ta 1.7           ppm Condie 1993
Granites 73 Ta 1.5           ppm Condie 1993
Granites 65 Tb 0.65           ppm Condie 1993
Granites 65 Tb 1.15           ppm Condie 1993
Granites 65 Tb 1.28           ppm Condie 1993
Granites 90 Th 18           ppm Condie 1993
Granites 90 Th 15           ppm Condie 1993
Granites 90 Th 18           ppm Condie 1993
Granites 22 Ti 0.25           wt%ox Condie 1993
Granites 22 Ti 0.25           wt%ox Condie 1993
Granites 22 Ti 0.28           wt%ox Condie 1993
Granites 92 U 5           ppm Condie 1993
Granites 92 U 4.5           ppm Condie 1993
Granites 92 U 3.5           ppm Condie 1993
Granites 23 V 15           ppm Condie 1993
Granites 23 V 18           ppm Condie 1993
Granites 23 V 20           ppm Condie 1993
Granites 39 Y 20           ppm Condie 1993
Granites 39 Y 45           ppm Condie 1993
Granites 39 Y 45           ppm Condie 1993
Granites 70 Yb 3.2           ppm Condie 1993
Granites 70 Yb 3.5           ppm Condie 1993
Granites 70 Yb 2           ppm Condie 1993
Granites 40 Zr 155           ppm Condie 1993
Granites 40 Zr 240           ppm Condie 1993
Granites 40 Zr 250           ppm Condie 1993
Graywackes 13 Al 15.5           wt%ox Condie 1993
Graywackes 13 Al 15.2           wt%ox Condie 1993
Graywackes 13 Al 15.5           wt%ox Condie 1993
Graywackes 13 Al 15.3           wt%ox Condie 1993
Graywackes 13 Al 15           wt%ox Condie 1993
Graywackes 13 Al 15.5           wt%ox Condie 1993
Graywackes 56 Ba 325           ppm Condie 1993
Graywackes 56 Ba 650           ppm Condie 1993
Graywackes 56 Ba 600           ppm Condie 1993
Graywackes 56 Ba 390           ppm Condie 1993
Graywackes 56 Ba 600           ppm Condie 1993
Graywackes 56 Ba 600           ppm Condie 1993
Graywackes 20 Ca 3.2           wt%ox Condie 1993
Graywackes 20 Ca 2.5           wt%ox Condie 1993
Graywackes 20 Ca 2.6           wt%ox Condie 1993
Graywackes 20 Ca 2.5           wt%ox Condie 1993
Graywackes 20 Ca 2.6           wt%ox Condie 1993
Graywackes 20 Ca 2.6           wt%ox Condie 1993
Graywackes 58 Ce 68           ppm Condie 1993
Graywackes 58 Ce 60           ppm Condie 1993
Graywackes 58 Ce 62           ppm Condie 1993
Graywackes 58 Ce 50           ppm Condie 1993
Graywackes 58 Ce 61           ppm Condie 1993
Graywackes 58 Ce 52           ppm Condie 1993
Graywackes 27 Co 20           ppm Condie 1993
Graywackes 27 Co 25           ppm Condie 1993
Graywackes 27 Co 30           ppm Condie 1993
Graywackes 27 Co 20           ppm Condie 1993
Graywackes 27 Co 28           ppm Condie 1993
Graywackes 27 Co 15           ppm Condie 1993
Graywackes 24 Cr 175           ppm Condie 1993
Graywackes 24 Cr 80           ppm Condie 1993
Graywackes 24 Cr 70           ppm Condie 1993
Graywackes 24 Cr 139           ppm Condie 1993
Graywackes 24 Cr 318           ppm Condie 1993
Graywackes 24 Cr 80           ppm Condie 1993
Graywackes 63 Eu 0.93           ppm Condie 1993
Graywackes 63 Eu 1.2           ppm Condie 1993
Graywackes 63 Eu 1.1           ppm Condie 1993
Graywackes 63 Eu 0.93           ppm Condie 1993
Graywackes 63 Eu 0.9           ppm Condie 1993
Graywackes 63 Eu 1.1           ppm Condie 1993
Graywackes   Eu/Eu* 0.62             Condie 1993
Graywackes   Eu/Eu* 0.89             Condie 1993
Graywackes   Eu/Eu* 0.73             Condie 1993
Graywackes   Eu/Eu* 0.89             Condie 1993
Graywackes   Eu/Eu* 0.62             Condie 1993
Graywackes   Eu/Eu* 0.6             Condie 1993
Graywackes 26 Fe 6.2           wt%ox Condie 1993
Graywackes 26 Fe 6.1           wt%ox Condie 1993
Graywackes 26 Fe 6.2           wt%ox Condie 1993
Graywackes 26 Fe 5.5           wt%ox Condie 1993
Graywackes 26 Fe 5.9           wt%ox Condie 1993
Graywackes 26 Fe 5.8           wt%ox Condie 1993
Graywackes 64 Gd 3.69           ppm Interpolated from Sm and Tb. Condie 1993
Graywackes 64 Gd 4.34           ppm Interpolated from Sm and Tb. Condie 1993
Graywackes 64 Gd 4.34           ppm Interpolated from Sm and Tb. Condie 1993
Graywackes 64 Gd 3.69           ppm Interpolated from Sm and Tb. Condie 1993
Graywackes 64 Gd 4.34           ppm Interpolated from Sm and Tb. Condie 1993
Graywackes 64 Gd 4.54           ppm Interpolated from Sm and Tb. Condie 1993
Graywackes 72 Hf 3.6           ppm Condie 1993
Graywackes 72 Hf 4.2           ppm Condie 1993
Graywackes 72 Hf 3.9           ppm Condie 1993
Graywackes 72 Hf 4           ppm Condie 1993
Graywackes 72 Hf 4           ppm Condie 1993
Graywackes 72 Hf 3.7           ppm Condie 1993
Graywackes 19 K 2.3           wt%ox Condie 1993
Graywackes 19 K 2.4           wt%ox Condie 1993
Graywackes 19 K 2.5           wt%ox Condie 1993
Graywackes 19 K 2           wt%ox Condie 1993
Graywackes 19 K 2.1           wt%ox Condie 1993
Graywackes 19 K 2.3           wt%ox Condie 1993
Graywackes 57 La 28           ppm Condie 1993
Graywackes 57 La 28           ppm Condie 1993
Graywackes 57 La 25           ppm Condie 1993
Graywackes 57 La 32           ppm Condie 1993
Graywackes 57 La 28           ppm Condie 1993
Graywackes 57 La 26           ppm Condie 1993
Graywackes   La[n]/Yb[n] 10.8             Condie 1993
Graywackes   La[n]/Yb[n] 10.8             Condie 1993
Graywackes   La[n]/Yb[n] 7.7             Condie 1993
Graywackes   La[n]/Yb[n] 11.3             Condie 1993
Graywackes   La[n]/Yb[n] 7.7             Condie 1993
Graywackes   La[n]/Yb[n] 7.7             Condie 1993
Graywackes 71 Lu 0.38           ppm Condie 1993
Graywackes 71 Lu 0.38           ppm Condie 1993
Graywackes 71 Lu 0.25           ppm Condie 1993
Graywackes 71 Lu 0.38           ppm Condie 1993
Graywackes 71 Lu 0.25           ppm Condie 1993
Graywackes 71 Lu 0.29           ppm Condie 1993
Graywackes 12 Mg 2.1           wt%ox Condie 1993
Graywackes 12 Mg 2.2           wt%ox Condie 1993
Graywackes 12 Mg 2           wt%ox Condie 1993
Graywackes 12 Mg 3.5           wt%ox Condie 1993
Graywackes 12 Mg 3.3           wt%ox Condie 1993
Graywackes 12 Mg 2.1           wt%ox Condie 1993
Graywackes 11 Na 3.1           wt%ox Condie 1993
Graywackes 11 Na 2.8           wt%ox Condie 1993
Graywackes 11 Na 2.9           wt%ox Condie 1993
Graywackes 11 Na 3.1           wt%ox Condie 1993
Graywackes 11 Na 2.8           wt%ox Condie 1993
Graywackes 11 Na 3           wt%ox Condie 1993
Graywackes 41 Nb 10           ppm Condie 1993
Graywackes 41 Nb 10           ppm Condie 1993
Graywackes 41 Nb 12           ppm Condie 1993
Graywackes 41 Nb 10           ppm Condie 1993
Graywackes 41 Nb 11           ppm Condie 1993
Graywackes 41 Nb 10           ppm Condie 1993
Graywackes 60 Nd 26           ppm Condie 1993
Graywackes 60 Nd 29           ppm Condie 1993
Graywackes 60 Nd 22           ppm Condie 1993
Graywackes 60 Nd 26           ppm Condie 1993
Graywackes 60 Nd 21           ppm Condie 1993
Graywackes 60 Nd 26           ppm Condie 1993
Graywackes 28 Ni 75           ppm Condie 1993
Graywackes 28 Ni 45           ppm Condie 1993
Graywackes 28 Ni 190           ppm Condie 1993
Graywackes 28 Ni 30           ppm Condie 1993
Graywackes 28 Ni 45           ppm Condie 1993
Graywackes 28 Ni 68           ppm Condie 1993
Graywackes 15 P 0.14           wt%ox Condie 1993
Graywackes 15 P 0.15           wt%ox Condie 1993
Graywackes 15 P 0.14           wt%ox Condie 1993
Graywackes 15 P 0.12           wt%ox Condie 1993
Graywackes 15 P 0.14           wt%ox Condie 1993
Graywackes 15 P 0.14           wt%ox Condie 1993
Graywackes 82 Pb 10           ppm Condie 1993
Graywackes 82 Pb 10           ppm Condie 1993
Graywackes 82 Pb 12           ppm Condie 1993
Graywackes 82 Pb 17           ppm Condie 1993
Graywackes 82 Pb 20           ppm Condie 1993
Graywackes 82 Pb 15           ppm Condie 1993
Graywackes 37 Rb 80           ppm Condie 1993
Graywackes 37 Rb 80           ppm Condie 1993
Graywackes 37 Rb 100           ppm Condie 1993
Graywackes 37 Rb 65           ppm Condie 1993
Graywackes 37 Rb 70           ppm Condie 1993
Graywackes 37 Rb 80           ppm Condie 1993
Graywackes 21 Sc 14           ppm Condie 1993
Graywackes 21 Sc 15           ppm Condie 1993
Graywackes 21 Sc 15           ppm Condie 1993
Graywackes 21 Sc 14           ppm Condie 1993
Graywackes 21 Sc 17           ppm Condie 1993
Graywackes 21 Sc 14           ppm Condie 1993
Graywackes 14 Si 65.4           wt%ox Condie 1993
Graywackes 14 Si 66.1           wt%ox Condie 1993
Graywackes 14 Si 66.1           wt%ox Condie 1993
Graywackes 14 Si 66.3           wt%ox Condie 1993
Graywackes 14 Si 65           wt%ox Condie 1993
Graywackes 14 Si 66.1           wt%ox Condie 1993
Graywackes 62 Sm 5.6           ppm Condie 1993
Graywackes 62 Sm 3.9           ppm Condie 1993
Graywackes 62 Sm 4.9           ppm Condie 1993
Graywackes 62 Sm 190           ppm Condie 1993
Graywackes 62 Sm 4.9           ppm Condie 1993
Graywackes 62 Sm 4.9           ppm Condie 1993
Graywackes 38 Sr 280           ppm Condie 1993
Graywackes 38 Sr 290           ppm Condie 1993
Graywackes 38 Sr 265           ppm Condie 1993
Graywackes 38 Sr 280           ppm Condie 1993
Graywackes 38 Sr 220           ppm Condie 1993
Graywackes 38 Sr 240           ppm Condie 1993
Graywackes 73 Ta 0.8           ppm Condie 1993
Graywackes 73 Ta 0.76           ppm Condie 1993
Graywackes 73 Ta 0.85           ppm Condie 1993
Graywackes 73 Ta 0.8           ppm Condie 1993
Graywackes 73 Ta 0.9           ppm Condie 1993
Graywackes 73 Ta 0.7           ppm Condie 1993
Graywackes 65 Tb 0.66           ppm Condie 1993
Graywackes 65 Tb 0.66           ppm Condie 1993
Graywackes 65 Tb 0.58           ppm Condie 1993
Graywackes 65 Tb 0.66           ppm Condie 1993
Graywackes 65 Tb 0.58           ppm Condie 1993
Graywackes 65 Tb 0.66           ppm Condie 1993
Graywackes 90 Th 8           ppm Condie 1993
Graywackes 90 Th 9           ppm Condie 1993
Graywackes 90 Th 8           ppm Condie 1993
Graywackes 90 Th 9           ppm Condie 1993
Graywackes 90 Th 8.5           ppm Condie 1993
Graywackes 90 Th 6           ppm Condie 1993
Graywackes 22 Ti 0.72           wt%ox Condie 1993
Graywackes 22 Ti 0.74           wt%ox Condie 1993
Graywackes 22 Ti 0.61           wt%ox Condie 1993
Graywackes 22 Ti 0.56           wt%ox Condie 1993
Graywackes 22 Ti 0.77           wt%ox Condie 1993
Graywackes 22 Ti 0.77           wt%ox Condie 1993
Graywackes 92 U 1.7           ppm Condie 1993
Graywackes 92 U 1.7           ppm Condie 1993
Graywackes 92 U 1.8           ppm Condie 1993
Graywackes 92 U 1.3           ppm Condie 1993
Graywackes 92 U 1.7           ppm Condie 1993
Graywackes 92 U 1.8           ppm Condie 1993
Graywackes 23 V 106           ppm Condie 1993
Graywackes 23 V 140           ppm Condie 1993
Graywackes 23 V 111           ppm Condie 1993
Graywackes 23 V 115           ppm Condie 1993
Graywackes 23 V 140           ppm Condie 1993
Graywackes 23 V 130           ppm Condie 1993
Graywackes 39 Y 28           ppm Condie 1993
Graywackes 39 Y 24           ppm Condie 1993
Graywackes 39 Y 27           ppm Condie 1993
Graywackes 39 Y 25           ppm Condie 1993
Graywackes 39 Y 25           ppm Condie 1993
Graywackes 39 Y 28           ppm Condie 1993
Graywackes 70 Yb 1.4           ppm Condie 1993
Graywackes 70 Yb 2.2           ppm Condie 1993
Graywackes 70 Yb 2.2           ppm Condie 1993
Graywackes 70 Yb 1.4           ppm Condie 1993
Graywackes 70 Yb 2.2           ppm Condie 1993
Graywackes 70 Yb 1.8           ppm Condie 1993
Graywackes 40 Zr 154           ppm Condie 1993
Graywackes 40 Zr 148           ppm Condie 1993
Graywackes 40 Zr 145           ppm Condie 1993
Graywackes 40 Zr 156           ppm Condie 1993
Graywackes 40 Zr 160           ppm Condie 1993
Graywackes 40 Zr 148           ppm Condie 1993
Komatiites 13 Al 7           wt%ox Condie 1993
Komatiites 56 Ba 8           ppm Condie 1993
Komatiites 20 Ca 6.5           wt%ox Condie 1993
Komatiites 58 Ce 1.7           ppm Condie 1993
Komatiites 27 Co 110           ppm Condie 1993
Komatiites 24 Cr 2700           ppm Condie 1993
Komatiites 63 Eu 0.26           ppm Condie 1993
Komatiites   Eu/Eu* 1.03             Condie 1993
Komatiites 26 Fe 9.9           wt%ox Condie 1993
Komatiites 64 Gd 0.96           ppm Interpolated from Sm and Tb. Condie 1993
Komatiites 72 Hf 1.5           ppm Condie 1993
Komatiites 19 K 0.05           wt%ox Condie 1993
Komatiites 57 La 0.5           ppm Condie 1993
Komatiites   La[n]/Yb[n] 0.4             Condie 1993
Komatiites 71 Lu 0.14           ppm Condie 1993
Komatiites 12 Mg 26           wt%ox Condie 1993
Komatiites 11 Na 0.2           wt%ox Condie 1993
Komatiites 41 Nb 0.7           ppm Condie 1993
Komatiites 60 Nd 1.7           ppm Condie 1993
Komatiites 28 Ni 1700           ppm Condie 1993
Komatiites 15 P 0.02           wt%ox Condie 1993
Komatiites 82 Pb 2           ppm Condie 1993
Komatiites 37 Rb 4           ppm Condie 1993
Komatiites 21 Sc 28           ppm Condie 1993
Komatiites 14 Si 47.8           wt%ox Condie 1993
Komatiites 62 Sm 0.63           ppm Condie 1993
Komatiites 38 Sr 11           ppm Condie 1993
Komatiites 73 Ta 0.05           ppm Condie 1993
Komatiites 65 Tb 0.19           ppm Condie 1993
Komatiites 90 Th 0.3           ppm Condie 1993
Komatiites 22 Ti 0.3           wt%ox Condie 1993
Komatiites 92 U 0.1           ppm Condie 1993
Komatiites 23 V 160           ppm Condie 1993
Komatiites 39 Y 8           ppm Condie 1993
Komatiites 70 Yb 0.84           ppm Condie 1993
Komatiites 40 Zr 35           ppm Condie 1993
Late Archean Upper Crust 13 Al 14.87           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust 13 Al 14.84           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust   Al2O3/SiO2 0.22             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust   Al2O3/SiO2 0.23             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust   Al2O3/TiO2 33             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust   Al2O3/TiO2 31             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust 56 Ba 576           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust 56 Ba 544           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust   Ba/La 19             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust   Ba/La 20             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust   Ba/Nb 64             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust   Ba/Nb 69             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust   Ba/Rb 7.4             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust   Ba/Rb 7.9             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust   Ba/Sr 2             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust   Ba/Sr 1.9             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust 20 Ca 3.8           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. CaO is that remaining after apatite is subtracted assuming all P2O5 is residing in apatite. Condie 1993
Late Archean Upper Crust 20 Ca 3.58           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. CaO is that remaining after apatite is subtracted assuming all P2O5 is residing in apatite. Condie 1993
Late Archean Upper Crust 58 Ce 56.8           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust 58 Ce 56           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust   CIW 54.6             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust   CIW 54.3             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust 27 Co 19           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust 27 Co 22           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust   Co/Th 2.4             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust   Co/Th 2.8             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust 24 Cr 140           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust 24 Cr 161           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust   Cr/Ni 1.8             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust   Cr/Ni 1.9             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust   Cr/Sc 13             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust   Cr/Sc 13             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust   Cr/Th 20             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust   Cr/Th 17             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust   Cr/V 1.9             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust   Cr/V 1.9             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust 63 Eu 0.99           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust 63 Eu 1           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust   Eu/Eu* 0.78             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust   Eu/Eu* 0.8             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust 26 Fe 4.88           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust 26 Fe 4.54           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust 64 Gd 3.58           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Interpolated from Sm and Tb. Condie 1993
Late Archean Upper Crust 64 Gd 3.74           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Interpolated from Sm and Tb. Condie 1993
Late Archean Upper Crust 72 Hf 3.9           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust 72 Hf 3.9           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust 19 K 2.51           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust 19 K 2.54           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust   K/Rb 288             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust   K/Rb 283             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust   K2O/Na2O 0.68             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust   K2O/Na2O 0.71             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust 57 La 28.7           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust 57 La 29.5           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust   La/Sc 2.8             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust   La/Sc 2.3             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust   La/Ta 42             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust   La/Ta 43             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust   La/Th 3.6             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust   La/Th 3.6             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust   La[n]/Yb[n] 11.5             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust   La[n]/Yb[n] 10.1             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust 71 Lu 0.26           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust 71 Lu 0.28           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust   Lu/Hf 0.072             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust   Lu/Hf 0.066             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust 12 Mg 2.89           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust 12 Mg 2.57           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust 11 Na 3.72           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust 11 Na 3.55           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust 41 Nb 8.5           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust 41 Nb 8.3           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust   Nb/Ta 12             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust   Nb/Ta 12             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust 60 Nd 25.1           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust 60 Nd 25.3           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust 28 Ni 76           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust 28 Ni 85           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust   Ni/Co 3.9             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust   Ni/Co 3.9             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust 15 P 0.11           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust 15 P 0.11           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust 82 Pb 18           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust 82 Pb 18           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust 37 Rb 73           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust 37 Rb 74           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust   Rb/Sr 0.28             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust   Rb/Sr 0.24             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust 21 Sc 10.7           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust 21 Sc 12.5           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust 14 Si 66.62           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust 14 Si 65.84           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust 62 Sm 4.03           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust 62 Sm 4.15           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust   Sm/Nd 0.164             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust   Sm/Nd 0.161             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust 38 Sr 267           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust 38 Sr 300           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust 73 Ta 0.69           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust 73 Ta 0.69           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust 65 Tb 0.55           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust 65 Tb 0.58           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust 90 Th 8.1           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust 90 Th 7.9           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust   Th/Nb 0.98             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust   Th/Nb 0.93             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust   Th/Sc 0.76             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust   Th/Sc 0.63             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust   Th/U 3.8             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust   Th/U 3.9             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust 22 Ti 0.48           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust 22 Ti 0.45           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust   Ti/Zr 19             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust   Ti/Zr 18             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust 92 U 2.1           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust 92 U 2.1           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust 23 V 73           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust 23 V 84           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust 39 Y 18           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust 39 Y 20           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust 70 Yb 1.72           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust 70 Yb 1.56           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust 40 Zr 150           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust 40 Zr 149           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Archean Upper Crust   Zr/Hf 38             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust   Zr/Hf 38             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust   Zr/Nb 17             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust   Zr/Nb 18             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust   Zr/Y 7.6             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Archean Upper Crust   Zr/Y 8.4             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust 13 Al 14.95           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust 13 Al 14.83           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust   Al2O3/SiO2 0.22             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust   Al2O3/SiO2 0.23             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust   Al2O3/TiO2 23             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust   Al2O3/TiO2 26             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust 56 Ba 690           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust 56 Ba 705           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust   Ba/La 24             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust   Ba/La 23             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust   Ba/Nb 60             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust   Ba/Nb 57             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust   Ba/Rb 6.9             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust   Ba/Rb 7.3             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust   Ba/Sr 2.4             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust   Ba/Sr 2.5             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust 20 Ca 3.49           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. CaO is that remaining after apatite is subtracted assuming all P2O5 is residing in apatite. Condie 1993
Late Proterozoic Upper Crust 20 Ca 3.18           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. CaO is that remaining after apatite is subtracted assuming all P2O5 is residing in apatite. Condie 1993
Late Proterozoic Upper Crust 58 Ce 59.8           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust 58 Ce 65.3           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust   CIW 56.6             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust   CIW 57.6             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust 27 Co 17           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust 27 Co 15           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust   Co/Th 1.8             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust   Co/Th 1.4             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust 24 Cr 47           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust 24 Cr 53           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust   Cr/Ni 1.8             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust   Cr/Ni 1.7             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust   Cr/Sc 3.3             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust   Cr/Sc 3.3             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust   Cr/Th 4.4             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust   Cr/Th 5.5             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust   Cr/V 0.53             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust   Cr/V 0.52             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust 63 Eu 1.1           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust 63 Eu 1.1           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust   Eu/Eu* 0.66             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust   Eu/Eu* 0.62             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust 26 Fe 4.69           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust 26 Fe 4.35           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust 64 Gd 5.24           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Interpolated from Sm and Tb. Condie 1993
Late Proterozoic Upper Crust 64 Gd 4.92           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Interpolated from Sm and Tb. Condie 1993
Late Proterozoic Upper Crust 72 Hf 4.9           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust 72 Hf 5.1           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust 19 K 3.05           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust 19 K 3.28           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust   K/Rb 267             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust   K/Rb 268             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust   K2O/Na2O 0.92             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust   K2O/Na2O 0.99             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust 57 La 28.7           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust 57 La 30.8           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust   La/Sc 1.8             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust   La/Sc 2.2             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust   La/Ta 32             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust   La/Ta 32             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust   La/Th 2.9             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust   La/Th 3             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust   La[n]/Yb[n] 7.8             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust   La[n]/Yb[n] 7.5             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust 71 Lu 0.39           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust 71 Lu 0.38           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust   Lu/Hf 0.077             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust   Lu/Hf 0.076             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust 12 Mg 1.82           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust 12 Mg 2.07           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust 11 Na 3.32           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust 11 Na 3.31           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust 41 Nb 11.6           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust 41 Nb 12.4           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust   Nb/Ta 13             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust   Nb/Ta 13             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust 60 Nd 27           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust 60 Nd 29.7           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust 28 Ni 30           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust 28 Ni 27           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust   Ni/Co 1.8             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust   Ni/Co 1.8             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust 15 P 0.13           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust 15 P 0.13           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust 82 Pb 17           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust 82 Pb 16           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust 37 Rb 102           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust 37 Rb 95           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust   Rb/Sr 0.36             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust   Rb/Sr 0.33             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust 21 Sc 15.7           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust 21 Sc 14.1           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust 14 Si 66.05           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust 14 Si 67.01           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust 62 Sm 5.33           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust 62 Sm 5.67           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust   Sm/Nd 0.198             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust   Sm/Nd 0.191             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust 38 Sr 281           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust 38 Sr 288           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust 73 Ta 0.9           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust 73 Ta 0.97           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust 65 Tb 0.77           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust 65 Tb 0.82           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust 90 Th 9.5           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust 90 Th 10.6           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust   Th/Nb 0.82             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust   Th/Nb 0.86             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust   Th/Sc 0.75             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust   Th/Sc 0.61             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust   Th/U 4             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust   Th/U 4             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust 22 Ti 0.58           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust 22 Ti 0.64           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust   Ti/Zr 22             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust   Ti/Zr 20             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust 92 U 2.4           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust 92 U 2.6           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust 23 V 101           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust 23 V 89           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust 39 Y 30           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust 39 Y 31           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust 70 Yb 2.4           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust 70 Yb 2.33           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust 40 Zr 172           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust 40 Zr 178           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Late Proterozoic Upper Crust   Zr/Hf 35             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust   Zr/Hf 35             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust   Zr/Nb 15             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust   Zr/Nb 14             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust   Zr/Y 5.7             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Late Proterozoic Upper Crust   Zr/Y 5.7             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust 13 Al 15.21           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust 13 Al 15.04           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust   Al2O3/SiO2 0.22             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust   Al2O3/SiO2 0.23             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust   Al2O3/TiO2 23             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust   Al2O3/TiO2 25             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust 56 Ba 707           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust 56 Ba 727           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust   Ba/La 28             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust   Ba/La 27             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust   Ba/Nb 62             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust   Ba/Nb 60             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust   Ba/Rb 7.5             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust   Ba/Rb 7.1             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust   Ba/Sr 2.8             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust   Ba/Sr 2.6             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust 20 Ca 3.94           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. CaO is that remaining after apatite is subtracted assuming all P2O5 is residing in apatite. Condie 1993
Mesozoic & Cenozoic Upper Crust 20 Ca 3.55           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. CaO is that remaining after apatite is subtracted assuming all P2O5 is residing in apatite. Condie 1993
Mesozoic & Cenozoic Upper Crust 58 Ce 59.3           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust 58 Ce 55.7           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust   CIW 56.1             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust   CIW 55             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust 27 Co 15           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust 27 Co 14           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust   Co/Th 1.7             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust   Co/Th 1.4             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust 24 Cr 50           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust 24 Cr 44           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust   Cr/Ni 1.9             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust   Cr/Ni 1.9             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust   Cr/Sc 3.1             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust   Cr/Sc 3.2             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust   Cr/Th 5.7             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust   Cr/Th 4.3             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust   Cr/V 0.47             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust   Cr/V 0.48             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust 63 Eu 1.02           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust 63 Eu 1.01           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust   Eu/Eu* 0.59             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust   Eu/Eu* 0.64             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust 26 Fe 4.59           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust 26 Fe 5.04           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust 64 Gd 5.11           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Interpolated from Sm and Tb. Condie 1993
Mesozoic & Cenozoic Upper Crust 64 Gd 4.81           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Interpolated from Sm and Tb. Condie 1993
Mesozoic & Cenozoic Upper Crust 72 Hf 4.5           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust 72 Hf 4.7           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust 19 K 3.11           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust 19 K 2.84           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust   K/Rb 250             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust   K/Rb 251             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust   K2O/Na2O 0.91             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust   K2O/Na2O 0.84             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust 57 La 27.3           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust 57 La 25.6           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust   La/Sc 1.9             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust   La/Sc 1.6             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust   La/Ta 28             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust   La/Ta 28             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust   La/Th 2.7             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust   La/Th 2.9             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust   La[n]/Yb[n] 6.7             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust   La[n]/Yb[n] 7             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust 71 Lu 0.43           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust 71 Lu 0.43           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust   Lu/Hf 0.096             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust   Lu/Hf 0.092             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust 12 Mg 2.21           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust 12 Mg 1.94           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust 11 Na 3.4           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust 11 Na 3.42           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust 41 Nb 12.2           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust 41 Nb 11.5           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust   Nb/Ta 13             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust   Nb/Ta 13             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust 60 Nd 24.6           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust 60 Nd 26.6           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust 28 Ni 23           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust 28 Ni 26           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust   Ni/Co 1.7             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust   Ni/Co 1.7             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust 15 P 0.13           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust 15 P 0.14           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust 82 Pb 17           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust 82 Pb 16           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust 37 Rb 103           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust 37 Rb 94           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust   Rb/Sr 0.35             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust   Rb/Sr 0.39             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust 21 Sc 14.2           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust 21 Sc 15.6           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust 14 Si 65.72           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust 14 Si 66.85           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust 62 Sm 5.43           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust 62 Sm 5.04           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust   Sm/Nd 0.205             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust   Sm/Nd 0.204             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust 38 Sr 262           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust 38 Sr 271           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust 73 Ta 0.96           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust 73 Ta 0.9           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust 65 Tb 0.8           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust 65 Tb 0.76           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust 90 Th 8.9           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust 90 Th 10.1           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust   Th/Nb 0.78             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust   Th/Nb 0.83             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust   Th/Sc 0.57             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust   Th/Sc 0.71             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust   Th/U 3.7             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust   Th/U 3.7             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust 22 Ti 0.66           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust 22 Ti 0.6           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust   Ti/Zr 21             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust   Ti/Zr 24             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust 92 U 2.7           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust 92 U 2.4           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust 23 V 93           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust 23 V 106           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust 39 Y 30           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust 39 Y 29           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust 70 Yb 2.36           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust 70 Yb 2.33           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust 40 Zr 167           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust 40 Zr 173           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Mesozoic & Cenozoic Upper Crust   Zr/Hf 37             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust   Zr/Hf 37             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust   Zr/Nb 14             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust   Zr/Nb 15             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust   Zr/Y 5.8             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Mesozoic & Cenozoic Upper Crust   Zr/Y 5.7             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust 13 Al 14.84           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust 13 Al 14.96           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust   Al2O3/SiO2 0.23             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust   Al2O3/SiO2 0.22             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust   Al2O3/TiO2 24             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust   Al2O3/TiO2 26             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust 56 Ba 701           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust 56 Ba 713           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust   Ba/La 24             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust   Ba/La 25             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust   Ba/Nb 60             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust   Ba/Nb 64             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust   Ba/Rb 7.2             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust   Ba/Rb 7.6             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust   Ba/Sr 2.4             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust   Ba/Sr 2.5             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust 20 Ca 3.17           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. CaO is that remaining after apatite is subtracted assuming all P2O5 is residing in apatite. Condie 1993
Middle Proterozoic Upper Crust 20 Ca 3.48           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. CaO is that remaining after apatite is subtracted assuming all P2O5 is residing in apatite. Condie 1993
Middle Proterozoic Upper Crust 58 Ce 64.3           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust 58 Ce 58.4           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust   CIW 57.7             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust   CIW 56.8             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust 27 Co 15           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust 27 Co 17           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust   Co/Th 1.5             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust   Co/Th 1.8             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust 24 Cr 55           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust 24 Cr 63           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust   Cr/Ni 1.9             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust   Cr/Ni 1.9             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust   Cr/Sc 4             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust   Cr/Sc 3.9             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust   Cr/Th 6.7             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust   Cr/Th 5.3             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust   Cr/V 0.63             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust   Cr/V 0.63             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust 63 Eu 1.18           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust 63 Eu 1.2           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust   Eu/Eu* 0.68             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust   Eu/Eu* 0.74             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust 26 Fe 4.8           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust 26 Fe 4.43           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust 64 Gd 4.85           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Interpolated from Sm and Tb. Condie 1993
Middle Proterozoic Upper Crust 64 Gd 5.19           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Interpolated from Sm and Tb. Condie 1993
Middle Proterozoic Upper Crust 72 Hf 5.1           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust 72 Hf 4.9           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust 19 K 3.02           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust 19 K 3.26           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust   K/Rb 272             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust   K/Rb 273             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust   K2O/Na2O 0.99             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust   K2O/Na2O 0.92             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust 57 La 30.3           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust 57 La 28           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust   La/Sc 1.8             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust   La/Sc 2.1             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust   La/Ta 33             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust   La/Ta 32             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust   La/Th 2.9             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust   La/Th 3             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust   La[n]/Yb[n] 7.8             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust   La[n]/Yb[n] 8.1             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust 71 Lu 0.35           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust 71 Lu 0.37           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust   Lu/Hf 0.072             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust   Lu/Hf 0.072             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust 12 Mg 1.87           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust 12 Mg 2.14           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust 11 Na 3.29           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust 11 Na 3.27           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust 41 Nb 11.9           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust 41 Nb 11           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust   Nb/Ta 13             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust   Nb/Ta 13             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust 60 Nd 26.1           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust 60 Nd 29.1           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust 28 Ni 29           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust 28 Ni 32           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust   Ni/Co 1.9             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust   Ni/Co 1.9             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust 15 P 0.13           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust 15 P 0.14           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust 82 Pb 17           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust 82 Pb 18           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust 37 Rb 92           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust 37 Rb 99           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust   Rb/Sr 0.31             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust   Rb/Sr 0.35             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust 21 Sc 15.8           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust 21 Sc 14.1           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust 14 Si 66.85           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust 14 Si 65.84           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust 62 Sm 5.19           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust 62 Sm 5.57           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust   Sm/Nd 0.199             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust   Sm/Nd 0.192             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust 38 Sr 294           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust 38 Sr 285           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust 73 Ta 0.86           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust 73 Ta 0.94           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust 65 Tb 0.81           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust 65 Tb 0.76           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust 90 Th 10.4           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust 90 Th 9.3           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust   Th/Nb 0.87             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust   Th/Nb 0.85             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust   Th/Sc 0.59             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust   Th/Sc 0.74             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust   Th/U 3.9             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust   Th/U 3.8             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust 22 Ti 0.63           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust 22 Ti 0.58           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust   Ti/Zr 19             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust   Ti/Zr 22             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust 92 U 2.7           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust 92 U 2.4           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust 23 V 99           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust 23 V 87           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust 39 Y 30           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust 39 Y 32           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust 70 Yb 2.18           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust 70 Yb 2.28           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust 40 Zr 173           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust 40 Zr 179           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Middle Proterozoic Upper Crust   Zr/Hf 35             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust   Zr/Hf 35             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust   Zr/Nb 16             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust   Zr/Nb 15             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust   Zr/Y 5.7             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Middle Proterozoic Upper Crust   Zr/Y 5.7             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
North American Shale Composite (NASC) 13 Al 16.9           wt%ox Major oxide and minor element compositions for North American Shale Composite. No source reference found in text.  Condie 1993
North American Shale Composite (NASC) 56 Ba 636           ppm Major oxide and minor element compositions for North American Shale Composite. No source reference found in text.  Condie 1993
North American Shale Composite (NASC) 20 Ca 3.63           wt%ox Major oxide and minor element compositions for North American Shale Composite. No source reference found in text.  Condie 1993
North American Shale Composite (NASC) 58 Ce 67           ppm Major oxide and minor element compositions for North American Shale Composite. No source reference found in text.  Condie 1993
North American Shale Composite (NASC) 27 Co 26           ppm Major oxide and minor element compositions for North American Shale Composite. No source reference found in text.  Condie 1993
North American Shale Composite (NASC) 24 Cr 125           ppm Major oxide and minor element compositions for North American Shale Composite. No source reference found in text.  Condie 1993
North American Shale Composite (NASC)   Cr/Th 10.2             Major ratio compositions for North American Shale Composite. No source reference found in text.  Condie 1993
North American Shale Composite (NASC) 63 Eu 1.2           ppm Major oxide and minor element compositions for North American Shale Composite. No source reference found in text.  Condie 1993
North American Shale Composite (NASC)   Eu/Eu* 0.68             Major ratio compositions for North American Shale Composite. No source reference found in text.  Condie 1993
North American Shale Composite (NASC) 26 Fe 5.67           wt%ox Major oxide and minor element compositions for North American Shale Composite. No source reference found in text.  Condie 1993
North American Shale Composite (NASC) 64 Gd 5.2           ppm Major oxide and minor element compositions for North American Shale Composite. No source reference found in text.  Condie 1993
North American Shale Composite (NASC) 72 Hf 6.3           ppm Major oxide and minor element compositions for North American Shale Composite. No source reference found in text.  Condie 1993
North American Shale Composite (NASC) 19 K 3.97           wt%ox Major oxide and minor element compositions for North American Shale Composite. No source reference found in text.  Condie 1993
North American Shale Composite (NASC) 57 La 31           ppm Major oxide and minor element compositions for North American Shale Composite. No source reference found in text.  Condie 1993
North American Shale Composite (NASC)   La/Sc 2.07             Major ratio compositions for North American Shale Composite. No source reference found in text.  Condie 1993
North American Shale Composite (NASC)   La[n]/Yb[n] 6.1             Major ratio compositions for North American Shale Composite. No source reference found in text.  Condie 1993
North American Shale Composite (NASC) 71 Lu 0.46           ppm Major oxide and minor element compositions for North American Shale Composite. No source reference found in text.  Condie 1993
North American Shale Composite (NASC) 12 Mg 2.86           wt%ox Major oxide and minor element compositions for North American Shale Composite. No source reference found in text.  Condie 1993
North American Shale Composite (NASC) 11 Na 1.14           wt%ox Major oxide and minor element compositions for North American Shale Composite. No source reference found in text.  Condie 1993
North American Shale Composite (NASC) 41 Nb 13           ppm Major oxide and minor element compositions for North American Shale Composite. No source reference found in text.  Condie 1993
North American Shale Composite (NASC) 60 Nd 27.4           ppm Major oxide and minor element compositions for North American Shale Composite. No source reference found in text.  Condie 1993
North American Shale Composite (NASC) 28 Ni 58           ppm Major oxide and minor element compositions for North American Shale Composite. No source reference found in text.  Condie 1993
North American Shale Composite (NASC) 15 P 0.13           wt%ox Major oxide and minor element compositions for North American Shale Composite. No source reference found in text.  Condie 1993
North American Shale Composite (NASC) 82 Pb 20           ppm Major oxide and minor element compositions for North American Shale Composite. No source reference found in text.  Condie 1993
North American Shale Composite (NASC) 37 Rb 125           ppm Major oxide and minor element compositions for North American Shale Composite. No source reference found in text.  Condie 1993
North American Shale Composite (NASC) 21 Sc 15           ppm Major oxide and minor element compositions for North American Shale Composite. No source reference found in text.  Condie 1993
North American Shale Composite (NASC) 14 Si 64.8           wt%ox Major oxide and minor element compositions for North American Shale Composite. No source reference found in text.  Condie 1993
North American Shale Composite (NASC) 62 Sm 5.6           ppm Major oxide and minor element compositions for North American Shale Composite. No source reference found in text.  Condie 1993
North American Shale Composite (NASC)   Sm/Nd 0.204             Major ratio compositions for North American Shale Composite. No source reference found in text.  Condie 1993
North American Shale Composite (NASC) 38 Sr 142           ppm Major oxide and minor element compositions for North American Shale Composite. No source reference found in text.  Condie 1993
North American Shale Composite (NASC) 73 Ta 1.1           ppm Major oxide and minor element compositions for North American Shale Composite. No source reference found in text.  Condie 1993
North American Shale Composite (NASC) 65 Tb 0.85           ppm Major oxide and minor element compositions for North American Shale Composite. No source reference found in text.  Condie 1993
North American Shale Composite (NASC) 90 Th 12.3           ppm Major oxide and minor element compositions for North American Shale Composite. No source reference found in text.  Condie 1993
North American Shale Composite (NASC)   Th/Sc 0.82             Major ratio compositions for North American Shale Composite. No source reference found in text.  Condie 1993
North American Shale Composite (NASC) 22 Ti 0.7           wt%ox Major oxide and minor element compositions for North American Shale Composite. No source reference found in text.  Condie 1993
North American Shale Composite (NASC) 92 U 2.7           ppm Major oxide and minor element compositions for North American Shale Composite. No source reference found in text.  Condie 1993
North American Shale Composite (NASC) 23 V 130           ppm Major oxide and minor element compositions for North American Shale Composite. No source reference found in text.  Condie 1993
North American Shale Composite (NASC) 39 Y 35           ppm Major oxide and minor element compositions for North American Shale Composite. No source reference found in text.  Condie 1993
North American Shale Composite (NASC) 70 Yb 3.1           ppm Major oxide and minor element compositions for North American Shale Composite. No source reference found in text.  Condie 1993
North American Shale Composite (NASC) 40 Zr 200           ppm Major oxide and minor element compositions for North American Shale Composite. No source reference found in text.  Condie 1993
Paleozoic Upper Crust 13 Al 14.99           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust 13 Al 15.15           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust   Al2O3/SiO2 0.22             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust   Al2O3/SiO2 0.23             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust   Al2O3/TiO2 24             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust   Al2O3/TiO2 22             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust 56 Ba 708           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust 56 Ba 683           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust   Ba/La 26             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust   Ba/La 27             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust   Ba/Nb 58             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust   Ba/Nb 59             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust   Ba/Rb 7.2             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust   Ba/Rb 7.7             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust   Ba/Sr 2.6             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust   Ba/Sr 2.8             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust 20 Ca 3.7           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. CaO is that remaining after apatite is subtracted assuming all P2O5 is residing in apatite. Condie 1993
Paleozoic Upper Crust 20 Ca 3.36           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. CaO is that remaining after apatite is subtracted assuming all P2O5 is residing in apatite. Condie 1993
Paleozoic Upper Crust 58 Ce 56.8           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust 58 Ce 60.2           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust   CIW 56.1             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust   CIW 57             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust 27 Co 14           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust 27 Co 16           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust   Co/Th 1.4             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust   Co/Th 1.8             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust 24 Cr 52           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust 24 Cr 45           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust   Cr/Ni 1.8             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust   Cr/Ni 1.8             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust   Cr/Sc 3.3             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust   Cr/Sc 3.2             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust   Cr/Th 5.8             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust   Cr/Th 4.5             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust   Cr/V 0.48             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust   Cr/V 0.47             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust 63 Eu 1.02           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust 63 Eu 1.01           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust   Eu/Eu* 0.65             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust   Eu/Eu* 0.6             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust 26 Fe 4.93           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust 26 Fe 4.51           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust 64 Gd 5.04           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Interpolated from Sm and Tb. Condie 1993
Paleozoic Upper Crust 64 Gd 4.71           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Interpolated from Sm and Tb. Condie 1993
Paleozoic Upper Crust 72 Hf 4.6           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust 72 Hf 4.4           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust 19 K 2.82           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust 19 K 3.1           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust   K/Rb 261             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust   K/Rb 263             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust   K2O/Na2O 0.93             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust   K2O/Na2O 0.85             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust 57 La 25.4           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust 57 La 27.1           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust   La/Sc 1.6             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust   La/Sc 1.9             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust   La/Ta 28             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust   La/Ta 28             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust   La/Th 2.7             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust   La/Th 2.9             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust   La[n]/Yb[n] 6.7             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust   La[n]/Yb[n] 7             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust 71 Lu 0.39           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust 71 Lu 0.38           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust   Lu/Hf 0.084             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust   Lu/Hf 0.086             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust 12 Mg 2.24           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust 12 Mg 1.96           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust 11 Na 3.32           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust 11 Na 3.35           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust 41 Nb 11.6           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust 41 Nb 12.3           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust   Nb/Ta 13             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust   Nb/Ta 13             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust 60 Nd 26           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust 60 Nd 27.6           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust 28 Ni 29           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust 28 Ni 26           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust   Ni/Co 1.8             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust   Ni/Co 1.8             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust 15 P 0.14           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust 15 P 0.13           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust 82 Pb 17           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust 82 Pb 16           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust 37 Rb 89           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust 37 Rb 99           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust   Rb/Sr 0.39             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust   Rb/Sr 0.34             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust 21 Sc 15.6           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust 21 Sc 14.2           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust 14 Si 66.79           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust 14 Si 65.65           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust 62 Sm 4.97           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust 62 Sm 5.38           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust   Sm/Nd 0.191             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust   Sm/Nd 0.195             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust 38 Sr 262           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust 38 Sr 256           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust 73 Ta 0.97           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust 73 Ta 0.9           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust 65 Tb 0.79           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust 65 Tb 0.74           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust 90 Th 8.9           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust 90 Th 10.1           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust   Th/Nb 0.82             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust   Th/Nb 0.77             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust   Th/Sc 0.71             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust   Th/Sc 0.57             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust   Th/U 3.8             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust   Th/U 3.8             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust 22 Ti 0.62           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust 22 Ti 0.68           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust   Ti/Zr 24             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust   Ti/Zr 21             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust 92 U 2.4           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust 92 U 2.7           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust 23 V 96           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust 23 V 109           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust 39 Y 30           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust 39 Y 31           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust 70 Yb 2.33           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust 70 Yb 2.29           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust 40 Zr 174           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust 40 Zr 168           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Condie 1993
Paleozoic Upper Crust   Zr/Hf 38             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust   Zr/Hf 38             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust   Zr/Nb 14             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust   Zr/Nb 15             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust   Zr/Y 5.5             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Paleozoic Upper Crust   Zr/Y 5.5             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Sandstones 13 Al 3.62           wt%ox Condie 1993
Sandstones 13 Al 4.28           wt%ox Condie 1993
Sandstones 13 Al 3.87           wt%ox Condie 1993
Sandstones 56 Ba 161           ppm Condie 1993
Sandstones 56 Ba 150           ppm Condie 1993
Sandstones 56 Ba 190           ppm Condie 1993
Sandstones 20 Ca 1.31           wt%ox Condie 1993
Sandstones 20 Ca 0.2           wt%ox Condie 1993
Sandstones 20 Ca 0.45           wt%ox Condie 1993
Sandstones 58 Ce 21.6           ppm Condie 1993
Sandstones 58 Ce 21           ppm Condie 1993
Sandstones 27 Co 2.8           ppm Condie 1993
Sandstones 27 Co 6.6           ppm Condie 1993
Sandstones 24 Cr 24           ppm Condie 1993
Sandstones 24 Cr 102           ppm Condie 1993
Sandstones 63 Eu 0.34           ppm Condie 1993
Sandstones 63 Eu 0.36           ppm Condie 1993
Sandstones   Eu/Eu* 0.68             Condie 1993
Sandstones   Eu/Eu* 0.88             Condie 1993
Sandstones 26 Fe 0.83           wt%ox Condie 1993
Sandstones 26 Fe 1.13           wt%ox Condie 1993
Sandstones 26 Fe 1.32           wt%ox Condie 1993
Sandstones 64 Gd 1.52           ppm Interpolated from Sm and Tb. Condie 1993
Sandstones 64 Gd 1.04           ppm Interpolated from Sm and Tb. Condie 1993
Sandstones 72 Hf 2.5           ppm Condie 1993
Sandstones 72 Hf 2.7           ppm Condie 1993
Sandstones 72 Hf 3.1           ppm Condie 1993
Sandstones 19 K 0.88           wt%ox Condie 1993
Sandstones 19 K 0.91           wt%ox Condie 1993
Sandstones 19 K 0.96           wt%ox Condie 1993
Sandstones 57 La 10.1           ppm Condie 1993
Sandstones 57 La 11.3           ppm Condie 1993
Sandstones 57 La 10.3           ppm Condie 1993
Sandstones   La[n]/Yb[n] 13.1             Condie 1993
Sandstones   La[n]/Yb[n] 7.3             Condie 1993
Sandstones 71 Lu 0.09           ppm Condie 1993
Sandstones 71 Lu 0.13           ppm Condie 1993
Sandstones 12 Mg 0.55           wt%ox Condie 1993
Sandstones 12 Mg 0.45           wt%ox Condie 1993
Sandstones 12 Mg 0.76           wt%ox Condie 1993
Sandstones 11 Na 0.51           wt%ox Condie 1993
Sandstones 11 Na 0.42           wt%ox Condie 1993
Sandstones 11 Na 0.32           wt%ox Condie 1993
Sandstones 41 Nb 4.1           ppm Condie 1993
Sandstones 41 Nb 4           ppm Condie 1993
Sandstones 41 Nb 3.7           ppm Condie 1993
Sandstones 60 Nd 9           ppm Condie 1993
Sandstones 60 Nd 9           ppm Condie 1993
Sandstones 28 Ni 23           ppm Condie 1993
Sandstones 28 Ni 11           ppm Condie 1993
Sandstones 15 P 0.02           wt%ox Condie 1993
Sandstones 15 P 0.03           wt%ox Condie 1993
Sandstones 15 P 0.02           wt%ox Condie 1993
Sandstones 82 Pb 19           ppm Condie 1993
Sandstones 82 Pb 20           ppm Condie 1993
Sandstones 82 Pb 19           ppm Condie 1993
Sandstones 37 Rb 30           ppm Condie 1993
Sandstones 37 Rb 32           ppm Condie 1993
Sandstones 37 Rb 25           ppm Condie 1993
Sandstones 21 Sc 2.4           ppm Condie 1993
Sandstones 21 Sc 1.6           ppm Condie 1993
Sandstones 14 Si 92.15           wt%ox Condie 1993
Sandstones 14 Si 91.5           wt%ox Condie 1993
Sandstones 14 Si 91.53           wt%ox Condie 1993
Sandstones 62 Sm 1.35           ppm Condie 1993
Sandstones 62 Sm 1.75           ppm Condie 1993
Sandstones 38 Sr 18           ppm Condie 1993
Sandstones 38 Sr 27           ppm Condie 1993
Sandstones 38 Sr 35           ppm Condie 1993
Sandstones 73 Ta 0.31           ppm Condie 1993
Sandstones 73 Ta 0.24           ppm Condie 1993
Sandstones 73 Ta 0.3           ppm Condie 1993
Sandstones 65 Tb 0.23           ppm Condie 1993
Sandstones 65 Tb 0.14           ppm Condie 1993
Sandstones 90 Th 4           ppm Condie 1993
Sandstones 90 Th 3.9           ppm Condie 1993
Sandstones 90 Th 4.2           ppm Condie 1993
Sandstones 22 Ti 0.4           wt%ox Condie 1993
Sandstones 22 Ti 0.25           wt%ox Condie 1993
Sandstones 22 Ti 0.17           wt%ox Condie 1993
Sandstones 92 U 1.1           ppm Condie 1993
Sandstones 92 U 1.1           ppm Condie 1993
Sandstones 92 U 1.2           ppm Condie 1993
Sandstones 23 V 11           ppm Condie 1993
Sandstones 23 V 29           ppm Condie 1993
Sandstones 39 Y 10.3           ppm Condie 1993
Sandstones 39 Y 5.8           ppm Condie 1993
Sandstones 39 Y 6.8           ppm Condie 1993
Sandstones 70 Yb 0.84           ppm Condie 1993
Sandstones 70 Yb 0.52           ppm Condie 1993
Sandstones 40 Zr 105           ppm Condie 1993
Sandstones 40 Zr 87           ppm Condie 1993
Sandstones 40 Zr 89           ppm Condie 1993
Shales 13 Al 17.8           wt%ox Condie 1993
Shales 13 Al 17.5           wt%ox Condie 1993
Shales 13 Al 17.5           wt%ox Condie 1993
Shales 56 Ba 456           ppm Condie 1993
Shales 56 Ba 642           ppm Condie 1993
Shales 56 Ba 551           ppm Condie 1993
Shales 20 Ca 1.3           wt%ox Condie 1993
Shales 20 Ca 0.64           wt%ox Condie 1993
Shales 20 Ca 0.71           wt%ox Condie 1993
Shales 58 Ce 82           ppm Condie 1993
Shales 58 Ce 60.9           ppm Condie 1993
Shales 58 Ce 81.7           ppm Condie 1993
Shales 27 Co 20           ppm Condie 1993
Shales 27 Co 18           ppm Condie 1993
Shales 27 Co 31           ppm Condie 1993
Shales 24 Cr 507           ppm Condie 1993
Shales 24 Cr 104           ppm Condie 1993
Shales 24 Cr 115           ppm Condie 1993
Shales   Cr/Th 59.6             Condie 1993
Shales   Cr/Th 7.7             Condie 1993
Shales   Cr/Th 8             Condie 1993
Shales 63 Eu 1.14           ppm Condie 1993
Shales 63 Eu 1.12           ppm Condie 1993
Shales 63 Eu 1.32           ppm Condie 1993
Shales   Eu/Eu* 0.73             Condie 1993
Shales   Eu/Eu* 0.66             Condie 1993
Shales   Eu/Eu* 0.64             Condie 1993
Shales 26 Fe 5.89           wt%ox Condie 1993
Shales 26 Fe 5.65           wt%ox Condie 1993
Shales 26 Fe 7.53           wt%ox Condie 1993
Shales 64 Gd 5.22           ppm Interpolated from Sm and Tb. Condie 1993
Shales 64 Gd 5.6           ppm Interpolated from Sm and Tb. Condie 1993
Shales 64 Gd 4.55           ppm Interpolated from Sm and Tb. Condie 1993
Shales 72 Hf 4.6           ppm Condie 1993
Shales 72 Hf 5.2           ppm Condie 1993
Shales 72 Hf 4.5           ppm Condie 1993
Shales 19 K 3.84           wt%ox Condie 1993
Shales 19 K 3.07           wt%ox Condie 1993
Shales 19 K 3.62           wt%ox Condie 1993
Shales 57 La 38.8           ppm Condie 1993
Shales 57 La 38           ppm Condie 1993
Shales 57 La 30.7           ppm Condie 1993
Shales   La/Sc 2.22             Condie 1993
Shales   La/Sc 1.5             Condie 1993
Shales   La/Sc 2.37             Condie 1993
Shales   La[n]/Yb[n] 8             Condie 1993
Shales   La[n]/Yb[n] 7.7             Condie 1993
Shales   La[n]/Yb[n] 8.1             Condie 1993
Shales 71 Lu 0.47           ppm Condie 1993
Shales 71 Lu 0.48           ppm Condie 1993
Shales 71 Lu 0.39           ppm Condie 1993
Shales 12 Mg 2.3           wt%ox Condie 1993
Shales 12 Mg 2.2           wt%ox Condie 1993
Shales 12 Mg 3.88           wt%ox Condie 1993
Shales 11 Na 0.68           wt%ox Condie 1993
Shales 11 Na 1.06           wt%ox Condie 1993
Shales 11 Na 1.1           wt%ox Condie 1993
Shales 41 Nb 11.3           ppm Condie 1993
Shales 41 Nb 15.4           ppm Condie 1993
Shales 41 Nb 16.8           ppm Condie 1993
Shales 60 Nd 37.5           ppm Condie 1993
Shales 60 Nd 32.3           ppm Condie 1993
Shales 60 Nd 27.7           ppm Condie 1993
Shales 28 Ni 52           ppm Condie 1993
Shales 28 Ni 54           ppm Condie 1993
Shales 28 Ni 221           ppm Condie 1993
Shales 15 P 0.14           wt%ox Condie 1993
Shales 15 P 0.1           wt%ox Condie 1993
Shales 15 P 0.12           wt%ox Condie 1993
Shales 82 Pb 22           ppm Condie 1993
Shales 82 Pb 27           ppm Condie 1993
Shales 82 Pb 13           ppm Condie 1993
Shales 37 Rb 163           ppm Condie 1993
Shales 37 Rb 165           ppm Condie 1993
Shales 37 Rb 111           ppm Condie 1993
Shales 21 Sc 16           ppm Condie 1993
Shales 21 Sc 17           ppm Condie 1993
Shales 21 Sc 21           ppm Condie 1993
Shales 14 Si 63.1           wt%ox Condie 1993
Shales 14 Si 63.6           wt%ox Condie 1993
Shales 14 Si 60.95           wt%ox Condie 1993
Shales 62 Sm 5.75           ppm Condie 1993
Shales 62 Sm 6.68           ppm Condie 1993
Shales 62 Sm 4.85           ppm Condie 1993
Shales   Sm/Nd 0.178             Condie 1993
Shales   Sm/Nd 0.175             Condie 1993
Shales   Sm/Nd 0.178             Condie 1993
Shales 38 Sr 108           ppm Condie 1993
Shales 38 Sr 61           ppm Condie 1993
Shales 38 Sr 136           ppm Condie 1993
Shales 73 Ta 0.84           ppm Condie 1993
Shales 73 Ta 1.4           ppm Condie 1993
Shales 73 Ta 1.4           ppm Condie 1993
Shales 65 Tb 0.9           ppm Condie 1993
Shales 65 Tb 0.71           ppm Condie 1993
Shales 65 Tb 0.81           ppm Condie 1993
Shales 90 Th 13.5           ppm Condie 1993
Shales 90 Th 8.5           ppm Condie 1993
Shales 90 Th 14.3           ppm Condie 1993
Shales 22 Ti 0.64           wt%ox Condie 1993
Shales 22 Ti 0.82           wt%ox Condie 1993
Shales 22 Ti 0.62           wt%ox Condie 1993
Shales   Ti/Sc 0.84             Condie 1993
Shales   Ti/Sc 0.41             Condie 1993
Shales   Ti/Sc 0.82             Condie 1993
Shales 92 U 2.9           ppm Condie 1993
Shales 92 U 2.4           ppm Condie 1993
Shales 92 U 3.4           ppm Condie 1993
Shales 23 V 117           ppm Condie 1993
Shales 23 V 154           ppm Condie 1993
Shales 23 V 100           ppm Condie 1993
Shales 39 Y 33           ppm Condie 1993
Shales 39 Y 28           ppm Condie 1993
Shales 39 Y 35           ppm Condie 1993
Shales 70 Yb 2.43           ppm Condie 1993
Shales 70 Yb 2.86           ppm Condie 1993
Shales 70 Yb 2.95           ppm Condie 1993
Shales 40 Zr 201           ppm Condie 1993
Shales 40 Zr 196           ppm Condie 1993
Shales 40 Zr 151           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 13 Al 15.5           wt%ox Condie 1993
Tonalites-Trondhjemites-Granodiorites 13 Al 15.6           wt%ox Condie 1993
Tonalites-Trondhjemites-Granodiorites 13 Al 15.1           wt%ox Condie 1993
Tonalites-Trondhjemites-Granodiorites 56 Ba 800           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 56 Ba 660           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 56 Ba 780           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 20 Ca 3.1           wt%ox Condie 1993
Tonalites-Trondhjemites-Granodiorites 20 Ca 3.5           wt%ox Condie 1993
Tonalites-Trondhjemites-Granodiorites 20 Ca 2.8           wt%ox Condie 1993
Tonalites-Trondhjemites-Granodiorites 58 Ce 47           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 58 Ce 45           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 58 Ce 56           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 27 Co 12           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 27 Co 10           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 27 Co 14           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 24 Cr 22           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 24 Cr 33           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 24 Cr 35           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 63 Eu 1.3           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 63 Eu 1           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 63 Eu 1.1           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites   Eu/Eu* 0.97             Condie 1993
Tonalites-Trondhjemites-Granodiorites   Eu/Eu* 0.93             Condie 1993
Tonalites-Trondhjemites-Granodiorites   Eu/Eu* 0.73             Condie 1993
Tonalites-Trondhjemites-Granodiorites 26 Fe 3.5           wt%ox Condie 1993
Tonalites-Trondhjemites-Granodiorites 26 Fe 3.8           wt%ox Condie 1993
Tonalites-Trondhjemites-Granodiorites 26 Fe 4.1           wt%ox Condie 1993
Tonalites-Trondhjemites-Granodiorites 64 Gd 2.98           ppm Interpolated from Sm and Tb. Condie 1993
Tonalites-Trondhjemites-Granodiorites 64 Gd 4.67           ppm Interpolated from Sm and Tb. Condie 1993
Tonalites-Trondhjemites-Granodiorites 64 Gd 4.09           ppm Interpolated from Sm and Tb. Condie 1993
Tonalites-Trondhjemites-Granodiorites 72 Hf 4           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 72 Hf 4.2           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 72 Hf 4.5           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 19 K 2.4           wt%ox Condie 1993
Tonalites-Trondhjemites-Granodiorites 19 K 3.3           wt%ox Condie 1993
Tonalites-Trondhjemites-Granodiorites 19 K 3.3           wt%ox Condie 1993
Tonalites-Trondhjemites-Granodiorites 57 La 26           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 57 La 25           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 57 La 30           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites   La[n]/Yb[n] 18.2             Condie 1993
Tonalites-Trondhjemites-Granodiorites   La[n]/Yb[n] 10.5             Condie 1993
Tonalites-Trondhjemites-Granodiorites   La[n]/Yb[n] 8.9             Condie 1993
Tonalites-Trondhjemites-Granodiorites 71 Lu 0.23           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 71 Lu 0.17           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 71 Lu 0.28           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 12 Mg 1.1           wt%ox Condie 1993
Tonalites-Trondhjemites-Granodiorites 12 Mg 1.7           wt%ox Condie 1993
Tonalites-Trondhjemites-Granodiorites 12 Mg 1.6           wt%ox Condie 1993
Tonalites-Trondhjemites-Granodiorites 11 Na 4.5           wt%ox Condie 1993
Tonalites-Trondhjemites-Granodiorites 11 Na 3.6           wt%ox Condie 1993
Tonalites-Trondhjemites-Granodiorites 11 Na 3.5           wt%ox Condie 1993
Tonalites-Trondhjemites-Granodiorites 41 Nb 9           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 41 Nb 7.5           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 41 Nb 8           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 60 Nd 22           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 60 Nd 19.5           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 60 Nd 20           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 28 Ni 13           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 28 Ni 15           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 28 Ni 15           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 15 P 0.11           wt%ox Condie 1993
Tonalites-Trondhjemites-Granodiorites 15 P 0.12           wt%ox Condie 1993
Tonalites-Trondhjemites-Granodiorites 15 P 0.13           wt%ox Condie 1993
Tonalites-Trondhjemites-Granodiorites 82 Pb 19           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 82 Pb 15           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 82 Pb 16           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 37 Rb 65           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 37 Rb 90           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 37 Rb 90           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 21 Sc 12           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 21 Sc 14           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 21 Sc 5           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 14 Si 66.8           wt%ox Condie 1993
Tonalites-Trondhjemites-Granodiorites 14 Si 67.2           wt%ox Condie 1993
Tonalites-Trondhjemites-Granodiorites 14 Si 69.5           wt%ox Condie 1993
Tonalites-Trondhjemites-Granodiorites 62 Sm 3.4           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 62 Sm 4.6           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 62 Sm 4.5           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 38 Sr 435           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 38 Sr 445           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 38 Sr 350           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 73 Ta 0.65           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 73 Ta 0.8           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 73 Ta 0.7           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 65 Tb 0.45           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 65 Tb 0.63           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 65 Tb 0.76           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 90 Th 10           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 90 Th 10           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 90 Th 8           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 22 Ti 0.55           wt%ox Condie 1993
Tonalites-Trondhjemites-Granodiorites 22 Ti 0.34           wt%ox Condie 1993
Tonalites-Trondhjemites-Granodiorites 22 Ti 0.53           wt%ox Condie 1993
Tonalites-Trondhjemites-Granodiorites 92 U 2           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 92 U 2.3           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 92 U 2.5           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 23 V 37           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 23 V 70           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 23 V 80           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 39 Y 13           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 39 Y 25           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 39 Y 25           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 70 Yb 1           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 70 Yb 1.7           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 70 Yb 1.5           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 40 Zr 160           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 40 Zr 140           ppm Condie 1993
Tonalites-Trondhjemites-Granodiorites 40 Zr 150           ppm Condie 1993
Upper Continental Crust 13 Al 14.96           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust 13 Al 14.87           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust   Al2O3/SiO2 0.22             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust   Al2O3/SiO2 0.23             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust   Al2O3/TiO2 28             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust   Al2O3/TiO2 27             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust 56 Ba 633           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust 56 Ba 626           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust   Ba/La 22             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust   Ba/La 22             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust   Ba/Nb 61             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust   Ba/Nb 64             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust   Ba/Rb 7.2             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust   Ba/Rb 7.7             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust   Ba/Sr 2.2             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust   Ba/Sr 2.3             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust 20 Ca 3.55           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. CaO is that remaining after apatite is subtracted assuming all P2O5 is residing in apatite. Condie 1993
Upper Continental Crust 20 Ca 3.6           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. CaO is that remaining after apatite is subtracted assuming all P2O5 is residing in apatite. Condie 1993
Upper Continental Crust 58 Ce 59.4           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust 58 Ce 57.5           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust   CIW 55.4             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust   CIW 55.7             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust 27 Co 18           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust 27 Co 18           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust   Co/Th 2.1             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust   Co/Th 2             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust 24 Cr 104           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust 24 Cr 112           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust   Cr/Ni 1.9             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust   Cr/Ni 1.8             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust   Cr/Sc 7.8             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust   Cr/Sc 8.4             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust   Cr/Th 12             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust   Cr/Th 12             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust   Cr/V 1.2             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust   Cr/V 1.3             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust 63 Eu 1.05           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust 63 Eu 1.05           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust   Eu/Eu* 0.74             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust   Eu/Eu* 0.7             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust 26 Fe 4.7           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust 26 Fe 4.68           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust 64 Gd 4.21           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Interpolated from Sm and Tb. Condie 1993
Upper Continental Crust 64 Gd 4.45           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Interpolated from Sm and Tb. Condie 1993
Upper Continental Crust 72 Hf 4.3           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust 72 Hf 4.4           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust 19 K 2.85           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust 19 K 2.73           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust   K/Rb 272             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust   K/Rb 275             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust   K2O/Na2O 0.78             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust   K2O/Na2O 0.83             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust 57 La 29           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust 57 La 28.4           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust   La/Sc 2.1             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust   La/Sc 2.2             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust   La/Ta 35             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust   La/Ta 36             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust   La/Th 3.3             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust   La/Th 3.2             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust   La[n]/Yb[n] 9             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust   La[n]/Yb[n] 8.7             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust 71 Lu 0.34           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust 71 Lu 0.32           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust   Lu/Hf 0.074             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust   Lu/Hf 0.076             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust 12 Mg 2.42           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust 12 Mg 2.46           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust 11 Na 3.43           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust 11 Na 3.51           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust 41 Nb 9.8           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust 41 Nb 10.3           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust   Nb/Ta 13             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust   Nb/Ta 12             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust 60 Nd 25.6           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust 60 Nd 26.9           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust 28 Ni 60           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust 28 Ni 56           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust   Ni/Co 3.3             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust   Ni/Co 3.1             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust 15 P 0.12           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust 15 P 0.12           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust 82 Pb 18           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust 82 Pb 17           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust 37 Rb 83           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust 37 Rb 87           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust   Rb/Sr 0.32             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust   Rb/Sr 0.29             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust 21 Sc 13.4           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust 21 Sc 13.3           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust 14 Si 66.21           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust 14 Si 66.33           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust 62 Sm 4.83           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust 62 Sm 4.59           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust   Sm/Nd 0.179             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust   Sm/Nd 0.179             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust 38 Sr 289           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust 38 Sr 269           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust 73 Ta 0.82           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust 73 Ta 0.79           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust 65 Tb 0.69           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust 65 Tb 0.66           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust 90 Th 9.1           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust 90 Th 8.6           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust   Th/Nb 0.88             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust   Th/Nb 0.88             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust   Th/Sc 0.65             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust   Th/Sc 0.68             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust   Th/U 3.8             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust   Th/U 3.9             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust 22 Ti 0.54           wt%ox Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust 22 Ti 0.55           wt%ox Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust   Ti/Zr 20             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust   Ti/Zr 20             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust 92 U 2.2           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust 92 U 2.4           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust 23 V 86           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust 23 V 86           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust 39 Y 25           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust 39 Y 24           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust 70 Yb 2.02           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust 70 Yb 1.91           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust 40 Zr 160           ppm Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust 40 Zr 162           ppm Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Condie 1993
Upper Continental Crust   Zr/Hf 37             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust   Zr/Hf 37             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust   Zr/Nb 16             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust   Zr/Nb 16             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust   Zr/Y 6.4             Restoration model. Concentrations are calculated after restoration of the amount of crust lost be erosion, in particular, important when estimating the composition of juvenile continental crust. The restoration is performed based on geologic maps and stratigraphic successions as summarized in Table 2. In this model 5 and 10 km extra crust is added to the present-day upper-crustal layer for Phanerozoic and Precambrian areas, respectively. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
Upper Continental Crust   Zr/Y 6.7             Map model. Concentrations are directly calculated from rock proportions scaled from geologic maps and stratigraphic successions as summarized in Table 2. The UCC is calculated from data in Tables 4-6 with a weight ratio for Archean:Proterozoic:Phanerozoic = 50:30:20 that can be further divided into 10% Early and 90% Late Archean; 50% Early and 25% Middle and 25% Late Proterozoic; and 50% Paleozoic and 50% Mesozoic-Cenozoic. Ratios calculated from weighted arithmetic means of rock types given in Appendix A-H. Condie 1993
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