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)
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 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 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   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 3.6           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 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 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 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   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 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 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   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/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/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 1.3             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   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 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 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   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   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 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 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 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 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 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 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 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 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   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   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   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   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 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 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   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/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/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/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/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] 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   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 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 0.076             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   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 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 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 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 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 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 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   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 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 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 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 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   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 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 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 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 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 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   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 13.3           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 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 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 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 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 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 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 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 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 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 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   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             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   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 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 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 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             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/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/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/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/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
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   147Sm/144Nd 0.116             Average Nd isotopic composition of Amazon, Changjiang and Mississippi river sediments which is found to have almost identical Nd isotopics than eroded upper continental crust. Esser & Turekian 1993 Goldstein & Jacobsen 1988
Goldstein et al. 1984
Upper Continental Crust   147Sm/144Nd 0.115             Average Sm/Nd isotopic composition of Amazon, Changjiang and Mississippi river sediments which is found to have almost identical Nd isotopics than eroded upper continental crust. For the sake of finding accurate Os ratios, these rivers comprise the representative values for global mean river sediment. Esser & Turekian 1993 Goldstein & Jacobsen 1988
Goldstein et al. 1984
Upper Continental Crust   187Os/186Os 10.54   0.12         Unweighted mean of multiple samples from deltaic or continental shelf sediments for this river which have purely terrigenous Os only. This mean includes loess sediments from the Mississippi river valley. This estimate can be used as a proxy for the upper continental crust. Esser & Turekian 1993
Upper Continental Crust   e-Nd -10.2             Average Nd isotopic composition of Amazon, Changjiang and Mississippi river sediments which is found to have almost identical Nd isotopics than eroded upper continental crust. Esser & Turekian 1993 Goldstein & Jacobsen 1988
Goldstein et al. 1984
Upper Continental Crust   e-Nd -11.4             Average Nd isotopic composition of Amazon, Changjiang and Mississippi river sediments which is found to have almost identical Nd isotopics than eroded upper continental crust. For the sake of finding accurate Os ratios, these rivers comprise the representative values for global mean river sediment. Esser & Turekian 1993 Goldstein & Jacobsen 1988
Goldstein et al. 1984
Upper Continental Crust   143Nd/144Nd 0.513077             Average isotopic composition of the Upper Crust as derived from composites taken from ODP sites 417/418. Values are taken from varying sources on the same composites in order to compare and contrast with 735B gabbroic isotopic composition which should closeley resemble 417/418. Hart et al. 1999 Staudigel et al. 1995
Smith et al. 1995
Hart & Staudigel 1989
Staudigel et al. 1989
Upper Continental Crust   87Sr/86Sr 0.704636             Average isotopic composition of the Upper Crust as derived from composites taken from ODP sites 417/418. Values are taken from varying sources on the same composites in order to compare and contrast with 735B gabbroic isotopic composition which should closeley resemble 417/418. Hart et al. 1999 Staudigel et al. 1995
Smith et al. 1995
Hart & Staudigel 1989
Staudigel et al. 1989
Upper Continental Crust 13 Al 15.53           wt%ox Average composition of the Upper Crust as derived from composites taken from ODP sites 417/418. Values are taken from varying sources on the same composites in order to compare and contrast with 735B gabbroic composition which should closeley resemble each other. Hart et al. 1999 Staudigel et al. 1995
Smith et al. 1995
Hart & Staudigel 1989
Staudigel et al. 1989
Upper Continental Crust 5 B 26.2           ppm Average composition of the Upper Crust as derived from composites taken from ODP sites 417/418. Values are taken from varying sources on the same composites in order to compare and contrast with 735B gabbroic composition which should closeley resemble each other. Hart et al. 1999 Staudigel et al. 1995
Smith et al. 1995
Hart & Staudigel 1989
Staudigel et al. 1989
Upper Continental Crust 56 Ba 16.85           ppm Average composition of the Upper Crust as derived from composites taken from ODP sites 417/418. Values are taken from varying sources on the same composites in order to compare and contrast with 735B gabbroic composition which should closeley resemble each other. Hart et al. 1999 Staudigel et al. 1995
Smith et al. 1995
Hart & Staudigel 1989
Staudigel et al. 1989
Upper Continental Crust 6 C 2.95           wt%ox Average composition of the Upper Crust as derived from composites taken from ODP sites 417/418. Values are taken from varying sources on the same composites in order to compare and contrast with 735B gabbroic composition which should closeley resemble each other. Hart et al. 1999 Staudigel et al. 1995
Smith et al. 1995
Hart & Staudigel 1989
Staudigel et al. 1989
Upper Continental Crust 20 Ca 12.88           wt%ox Average composition of the Upper Crust as derived from composites taken from ODP sites 417/418. Values are taken from varying sources on the same composites in order to compare and contrast with 735B gabbroic composition which should closeley resemble each other. Hart et al. 1999 Staudigel et al. 1995
Smith et al. 1995
Hart & Staudigel 1989
Staudigel et al. 1989
Upper Continental Crust 58 Ce 6.19           ppm Average composition of the Upper Crust as derived from composites taken from ODP sites 417/418. Values are taken from varying sources on the same composites in order to compare and contrast with 735B gabbroic composition which should closeley resemble each other. Hart et al. 1999 Staudigel et al. 1995
Smith et al. 1995
Hart & Staudigel 1989
Staudigel et al. 1989
Upper Continental Crust 55 Cs 0.173           ppm Average composition of the Upper Crust as derived from composites taken from ODP sites 417/418. Values are taken from varying sources on the same composites in order to compare and contrast with 735B gabbroic composition which should closeley resemble each other. Hart et al. 1999 Staudigel et al. 1995
Smith et al. 1995
Hart & Staudigel 1989
Staudigel et al. 1989
Upper Continental Crust   d11B 0.8             Average isotopic composition of the Upper Crust as derived from composites taken from ODP sites 417/418. Values are taken from varying sources on the same composites in order to compare and contrast with 735B gabbroic isotopic composition which should closeley resemble 417/418. Hart et al. 1999 Staudigel et al. 1995
Smith et al. 1995
Hart & Staudigel 1989
Staudigel et al. 1989
Upper Continental Crust   d18O 9.96             Average isotopic composition of the Upper Crust as derived from composites taken from ODP sites 417/418. Values are taken from varying sources on the same composites in order to compare and contrast with 735B gabbroic isotopic composition which should closeley resemble 417/418. Hart et al. 1999 Staudigel et al. 1995
Smith et al. 1995
Hart & Staudigel 1989
Staudigel et al. 1989
Upper Continental Crust 63 Eu 0.93           ppm Average composition of the Upper Crust as derived from composites taken from ODP sites 417/418. Values are taken from varying sources on the same composites in order to compare and contrast with 735B gabbroic composition which should closeley resemble each other. Hart et al. 1999 Staudigel et al. 1995
Smith et al. 1995
Hart & Staudigel 1989
Staudigel et al. 1989
Upper Continental Crust   Eu/Eu* 0.871             Elemental ratios of the Upper Crust as derived from composites taken from ODP sites 417/418. Values are taken from varying sources on the same composites in order to compare and contrast with 735B gabbroic composition which should closeley resemble each other. Hart et al. 1999 Staudigel et al. 1995
Smith et al. 1995
Hart & Staudigel 1989
Staudigel et al. 1989
Upper Continental Crust 26 Fe 9.02           wt%ox Average composition of the Upper Crust as derived from composites taken from ODP sites 417/418. Values are taken from varying sources on the same composites in order to compare and contrast with 735B gabbroic composition which should closeley resemble each other. Hart et al. 1999 Staudigel et al. 1995
Smith et al. 1995
Hart & Staudigel 1989
Staudigel et al. 1989
Upper Continental Crust 1 H 2.68           wt%ox Average composition of the Upper Crust as derived from composites taken from ODP sites 417/418. Values are taken from varying sources on the same composites in order to compare and contrast with 735B gabbroic composition which should closeley resemble each other. Hart et al. 1999 Staudigel et al. 1995
Smith et al. 1995
Hart & Staudigel 1989
Staudigel et al. 1989
Upper Continental Crust 19 K 4805           ppm Average composition of the Upper Crust as derived from composites taken from ODP sites 417/418. Values are taken from varying sources on the same composites in order to compare and contrast with 735B gabbroic composition which should closeley resemble each other. Hart et al. 1999 Staudigel et al. 1995
Smith et al. 1995
Hart & Staudigel 1989
Staudigel et al. 1989
Upper Continental Crust 19 K 0.56           wt%ox Average composition of the Upper Crust as derived from composites taken from ODP sites 417/418. Values are taken from varying sources on the same composites in order to compare and contrast with 735B gabbroic composition which should closeley resemble each other. Hart et al. 1999 Staudigel et al. 1995
Smith et al. 1995
Hart & Staudigel 1989
Staudigel et al. 1989
Upper Continental Crust 57 La 1.97           ppm Average composition of the Upper Crust as derived from composites taken from ODP sites 417/418. Values are taken from varying sources on the same composites in order to compare and contrast with 735B gabbroic composition which should closeley resemble each other. Hart et al. 1999 Staudigel et al. 1995
Smith et al. 1995
Hart & Staudigel 1989
Staudigel et al. 1989
Upper Continental Crust 71 Lu 0.44           ppm Average composition of the Upper Crust as derived from composites taken from ODP sites 417/418. Values are taken from varying sources on the same composites in order to compare and contrast with 735B gabbroic composition which should closeley resemble each other. Hart et al. 1999 Staudigel et al. 1995
Smith et al. 1995
Hart & Staudigel 1989
Staudigel et al. 1989
Upper Continental Crust 12 Mg 56.82             Average composition of the Upper Crust as derived from composites taken from ODP sites 417/418. Values are taken from varying sources on the same composites in order to compare and contrast with 735B gabbroic composition which should closeley resemble each other. Hart et al. 1999 Staudigel et al. 1995
Smith et al. 1995
Hart & Staudigel 1989
Staudigel et al. 1989
Upper Continental Crust 12 Mg 6.66           wt%ox Average composition of the Upper Crust as derived from composites taken from ODP sites 417/418. Values are taken from varying sources on the same composites in order to compare and contrast with 735B gabbroic composition which should closeley resemble each other. Hart et al. 1999 Staudigel et al. 1995
Smith et al. 1995
Hart & Staudigel 1989
Staudigel et al. 1989
Upper Continental Crust 25 Mn 0.17           wt%ox Average composition of the Upper Crust as derived from composites taken from ODP sites 417/418. Values are taken from varying sources on the same composites in order to compare and contrast with 735B gabbroic composition which should closeley resemble each other. Hart et al. 1999 Staudigel et al. 1995
Smith et al. 1995
Hart & Staudigel 1989
Staudigel et al. 1989
Upper Continental Crust 11 Na 2.07           wt%ox Average composition of the Upper Crust as derived from composites taken from ODP sites 417/418. Values are taken from varying sources on the same composites in order to compare and contrast with 735B gabbroic composition which should closeley resemble each other. Hart et al. 1999 Staudigel et al. 1995
Smith et al. 1995
Hart & Staudigel 1989
Staudigel et al. 1989
Upper Continental Crust 41 Nb 3           ppm Average composition of the Upper Crust as derived from composites taken from ODP sites 417/418. Values are taken from varying sources on the same composites in order to compare and contrast with 735B gabbroic composition which should closeley resemble each other. Hart et al. 1999 Staudigel et al. 1995
Smith et al. 1995
Hart & Staudigel 1989
Staudigel et al. 1989
Upper Continental Crust 60 Nd 6.76           ppm Average composition of the Upper Crust as derived from composites taken from ODP sites 417/418. Values are taken from varying sources on the same composites in order to compare and contrast with 735B gabbroic composition which should closeley resemble each other. Hart et al. 1999 Staudigel et al. 1995
Smith et al. 1995
Hart & Staudigel 1989
Staudigel et al. 1989
Upper Continental Crust 15 P 0.11           wt%ox Average composition of the Upper Crust as derived from composites taken from ODP sites 417/418. Values are taken from varying sources on the same composites in order to compare and contrast with 735B gabbroic composition which should closeley resemble each other. Hart et al. 1999 Staudigel et al. 1995
Smith et al. 1995
Hart & Staudigel 1989
Staudigel et al. 1989
Upper Continental Crust 82 Pb 0.69           ppm Average composition of the Upper Crust as derived from composites taken from ODP sites 417/418. Values are taken from varying sources on the same composites in order to compare and contrast with 735B gabbroic composition which should closeley resemble each other. Hart et al. 1999 Staudigel et al. 1995
Smith et al. 1995
Hart & Staudigel 1989
Staudigel et al. 1989
Upper Continental Crust 37 Rb 9.04           ppm Average composition of the Upper Crust as derived from composites taken from ODP sites 417/418. Values are taken from varying sources on the same composites in order to compare and contrast with 735B gabbroic composition which should closeley resemble each other. Hart et al. 1999 Staudigel et al. 1995
Smith et al. 1995
Hart & Staudigel 1989
Staudigel et al. 1989
Upper Continental Crust   Rb/Cs 52.3             Elemental ratios of the Upper Crust as derived from composites taken from ODP sites 417/418. Values are taken from varying sources on the same composites in order to compare and contrast with 735B gabbroic composition which should closeley resemble each other. Hart et al. 1999 Staudigel et al. 1995
Smith et al. 1995
Hart & Staudigel 1989
Staudigel et al. 1989
Upper Continental Crust 14 Si 45.8           wt%ox Average composition of the Upper Crust as derived from composites taken from ODP sites 417/418. Values are taken from varying sources on the same composites in order to compare and contrast with 735B gabbroic composition which should closeley resemble each other. Hart et al. 1999 Staudigel et al. 1995
Smith et al. 1995
Hart & Staudigel 1989
Staudigel et al. 1989
Upper Continental Crust 62 Sm 2.552           ppm Average composition of the Upper Crust as derived from composites taken from ODP sites 417/418. Values are taken from varying sources on the same composites in order to compare and contrast with 735B gabbroic composition which should closeley resemble each other. Hart et al. 1999 Staudigel et al. 1995
Smith et al. 1995
Hart & Staudigel 1989
Staudigel et al. 1989
Upper Continental Crust 38 Sr 117.5           ppm Average composition of the Upper Crust as derived from composites taken from ODP sites 417/418. Values are taken from varying sources on the same composites in order to compare and contrast with 735B gabbroic composition which should closeley resemble each other. Hart et al. 1999 Staudigel et al. 1995
Smith et al. 1995
Hart & Staudigel 1989
Staudigel et al. 1989
Upper Continental Crust   Sr/Sr* 1.01             Elemental ratios of the Upper Crust as derived from composites taken from ODP sites 417/418. Values are taken from varying sources on the same composites in order to compare and contrast with 735B gabbroic composition which should closeley resemble each other. Hart et al. 1999 Staudigel et al. 1995
Smith et al. 1995
Hart & Staudigel 1989
Staudigel et al. 1989
Upper Continental Crust 65 Tb 0.75           ppm Average composition of the Upper Crust as derived from composites taken from ODP sites 417/418. Values are taken from varying sources on the same composites in order to compare and contrast with 735B gabbroic composition which should closeley resemble each other. Hart et al. 1999 Staudigel et al. 1995
Smith et al. 1995
Hart & Staudigel 1989
Staudigel et al. 1989
Upper Continental Crust 90 Th 0.0723           ppm Average composition of the Upper Crust as derived from composites taken from ODP sites 417/418. Values are taken from varying sources on the same composites in order to compare and contrast with 735B gabbroic composition which should closeley resemble each other. Hart et al. 1999 Staudigel et al. 1995
Smith et al. 1995
Hart & Staudigel 1989
Staudigel et al. 1989
Upper Continental Crust   Th/U 0.225             Elemental ratios of the Upper Crust as derived from composites taken from ODP sites 417/418. Values are taken from varying sources on the same composites in order to compare and contrast with 735B gabbroic composition which should closeley resemble each other. Hart et al. 1999 Staudigel et al. 1995
Smith et al. 1995
Hart & Staudigel 1989
Staudigel et al. 1989
Upper Continental Crust 22 Ti 1.12           wt%ox Average composition of the Upper Crust as derived from composites taken from ODP sites 417/418. Values are taken from varying sources on the same composites in order to compare and contrast with 735B gabbroic composition which should closeley resemble each other. Hart et al. 1999 Staudigel et al. 1995
Smith et al. 1995
Hart & Staudigel 1989
Staudigel et al. 1989
Upper Continental Crust   Ti/Ti* 0.804             Elemental ratios of the Upper Crust as derived from composites taken from ODP sites 417/418. Values are taken from varying sources on the same composites in order to compare and contrast with 735B gabbroic composition which should closeley resemble each other. Hart et al. 1999 Staudigel et al. 1995
Smith et al. 1995
Hart & Staudigel 1989
Staudigel et al. 1989
Upper Continental Crust 92 U 0.321           ppm Average composition of the Upper Crust as derived from composites taken from ODP sites 417/418. Values are taken from varying sources on the same composites in order to compare and contrast with 735B gabbroic composition which should closeley resemble each other. Hart et al. 1999 Staudigel et al. 1995
Smith et al. 1995
Hart & Staudigel 1989
Staudigel et al. 1989
Upper Continental Crust   U/Pb 0.465             Elemental ratios of the Upper Crust as derived from composites taken from ODP sites 417/418. Values are taken from varying sources on the same composites in order to compare and contrast with 735B gabbroic composition which should closeley resemble each other. Hart et al. 1999 Staudigel et al. 1995
Smith et al. 1995
Hart & Staudigel 1989
Staudigel et al. 1989
Upper Continental Crust 39 Y 32           ppm Average composition of the Upper Crust as derived from composites taken from ODP sites 417/418. Values are taken from varying sources on the same composites in order to compare and contrast with 735B gabbroic composition which should closeley resemble each other. Hart et al. 1999 Staudigel et al. 1995
Smith et al. 1995
Hart & Staudigel 1989
Staudigel et al. 1989
Upper Continental Crust 70 Yb 2.82           ppm Average composition of the Upper Crust as derived from composites taken from ODP sites 417/418. Values are taken from varying sources on the same composites in order to compare and contrast with 735B gabbroic composition which should closeley resemble each other. Hart et al. 1999 Staudigel et al. 1995
Smith et al. 1995
Hart & Staudigel 1989
Staudigel et al. 1989
Upper Continental Crust 40 Zr 67           ppm Average composition of the Upper Crust as derived from composites taken from ODP sites 417/418. Values are taken from varying sources on the same composites in order to compare and contrast with 735B gabbroic composition which should closeley resemble each other. Hart et al. 1999 Staudigel et al. 1995
Smith et al. 1995
Hart & Staudigel 1989
Staudigel et al. 1989
Upper Continental Crust   (Gd/Yb)(N) 1.65             Major and minor element composition of the Upper Crust of the Earth with selected trace element ratios as given by Rudnick and Gao 2004. Kemp & Hawkesworth 2004 Rudnick & Gao 2004
Upper Continental Crust 13 Al 15.4           wt% Major and minor element composition of the Upper Crust of the Earth with selected trace element ratios as given by Rudnick and Gao 2004. Kemp & Hawkesworth 2004 Rudnick & Gao 2004
Upper Continental Crust 56 Ba 628           ppm Major and minor element composition of the Upper Crust of the Earth with selected trace element ratios as given by Rudnick and Gao 2004. Kemp & Hawkesworth 2004 Rudnick & Gao 2004
Upper Continental Crust 20 Ca 3.59           wt% Major and minor element composition of the Upper Crust of the Earth with selected trace element ratios as given by Rudnick and Gao 2004. Kemp & Hawkesworth 2004 Rudnick & Gao 2004
Upper Continental Crust 58 Ce 63           ppm Major and minor element composition of the Upper Crust of the Earth with selected trace element ratios as given by Rudnick and Gao 2004. Kemp & Hawkesworth 2004 Rudnick & Gao 2004
Upper Continental Crust 27 Co 17.3           ppm Major and minor element composition of the Upper Crust of the Earth with selected trace element ratios as given by Rudnick and Gao 2004. Kemp & Hawkesworth 2004 Rudnick & Gao 2004
Upper Continental Crust 24 Cr 92           ppm Major and minor element composition of the Upper Crust of the Earth with selected trace element ratios as given by Rudnick and Gao 2004. Kemp & Hawkesworth 2004 Rudnick & Gao 2004
Upper Continental Crust 29 Cu 28           ppm Major and minor element composition of the Upper Crust of the Earth with selected trace element ratios as given by Rudnick and Gao 2004. Kemp & Hawkesworth 2004 Rudnick & Gao 2004
Upper Continental Crust 66 Dy 3.9           ppm Major and minor element composition of the Upper Crust of the Earth with selected trace element ratios as given by Rudnick and Gao 2004. Kemp & Hawkesworth 2004 Rudnick & Gao 2004
Upper Continental Crust 68 Er 2.3           ppm Major and minor element composition of the Upper Crust of the Earth with selected trace element ratios as given by Rudnick and Gao 2004. Kemp & Hawkesworth 2004 Rudnick & Gao 2004
Upper Continental Crust 63 Eu 1           ppm Major and minor element composition of the Upper Crust of the Earth with selected trace element ratios as given by Rudnick and Gao 2004. Kemp & Hawkesworth 2004 Rudnick & Gao 2004
Upper Continental Crust   Eu/Eu* 0.72             Major and minor element composition of the Upper Crust of the Earth with selected trace element ratios as given by Rudnick and Gao 2004. Kemp & Hawkesworth 2004 Rudnick & Gao 2004
Upper Continental Crust   Eu/Sr 0.0031             Major and minor element composition of the Upper Crust of the Earth with selected trace element ratios as given by Rudnick and Gao 2004. Kemp & Hawkesworth 2004 Rudnick & Gao 2004
Upper Continental Crust 26 Fe 5.04           wt% Major and minor element composition of the Upper Crust of the Earth with selected trace element ratios as given by Rudnick and Gao 2004. Kemp & Hawkesworth 2004 Rudnick & Gao 2004
Upper Continental Crust 31 Ga 17.5           ppm Major and minor element composition of the Upper Crust of the Earth with selected trace element ratios as given by Rudnick and Gao 2004. Kemp & Hawkesworth 2004 Rudnick & Gao 2004
Upper Continental Crust 64 Gd 4           ppm Major and minor element composition of the Upper Crust of the Earth with selected trace element ratios as given by Rudnick and Gao 2004. Kemp & Hawkesworth 2004 Rudnick & Gao 2004
Upper Continental Crust 72 Hf 5.3           ppm Major and minor element composition of the Upper Crust of the Earth with selected trace element ratios as given by Rudnick and Gao 2004. Kemp & Hawkesworth 2004 Rudnick & Gao 2004
Upper Continental Crust 67 Ho 0.83           ppm Major and minor element composition of the Upper Crust of the Earth with selected trace element ratios as given by Rudnick and Gao 2004. Kemp & Hawkesworth 2004 Rudnick & Gao 2004
Upper Continental Crust 19 K 2.8           wt% Major and minor element composition of the Upper Crust of the Earth with selected trace element ratios as given by Rudnick and Gao 2004. Kemp & Hawkesworth 2004 Rudnick & Gao 2004
Upper Continental Crust 57 La 31           ppm Major and minor element composition of the Upper Crust of the Earth with selected trace element ratios as given by Rudnick and Gao 2004. Kemp & Hawkesworth 2004 Rudnick & Gao 2004
Upper Continental Crust 71 Lu 0.31           ppm Major and minor element composition of the Upper Crust of the Earth with selected trace element ratios as given by Rudnick and Gao 2004. Kemp & Hawkesworth 2004 Rudnick & Gao 2004
Upper Continental Crust 12 Mg 2.48           wt% Major and minor element composition of the Upper Crust of the Earth with selected trace element ratios as given by Rudnick and Gao 2004. Kemp & Hawkesworth 2004 Rudnick & Gao 2004
Upper Continental Crust   Mg# 46.7             Major and minor element composition of the Upper Crust of the Earth with selected trace element ratios as given by Rudnick and Gao 2004. Kemp & Hawkesworth 2004 Rudnick & Gao 2004
Upper Continental Crust 25 Mn 0.1           wt% Major and minor element composition of the Upper Crust of the Earth with selected trace element ratios as given by Rudnick and Gao 2004. Kemp & Hawkesworth 2004 Rudnick & Gao 2004
Upper Continental Crust 11 Na 3.27           wt% Major and minor element composition of the Upper Crust of the Earth with selected trace element ratios as given by Rudnick and Gao 2004. Kemp & Hawkesworth 2004 Rudnick & Gao 2004
Upper Continental Crust 41 Nb 12           ppm Major and minor element composition of the Upper Crust of the Earth with selected trace element ratios as given by Rudnick and Gao 2004. Kemp & Hawkesworth 2004 Rudnick & Gao 2004
Upper Continental Crust 60 Nd 27           ppm Major and minor element composition of the Upper Crust of the Earth with selected trace element ratios as given by Rudnick and Gao 2004. Kemp & Hawkesworth 2004 Rudnick & Gao 2004
Upper Continental Crust 28 Ni 47           ppm Major and minor element composition of the Upper Crust of the Earth with selected trace element ratios as given by Rudnick and Gao 2004. Kemp & Hawkesworth 2004 Rudnick & Gao 2004
Upper Continental Crust 15 P 0.15           wt% Major and minor element composition of the Upper Crust of the Earth with selected trace element ratios as given by Rudnick and Gao 2004. Kemp & Hawkesworth 2004 Rudnick & Gao 2004
Upper Continental Crust 82 Pb 17           ppm Major and minor element composition of the Upper Crust of the Earth with selected trace element ratios as given by Rudnick and Gao 2004. Kemp & Hawkesworth 2004 Rudnick & Gao 2004
Upper Continental Crust 59 Pr 7.1           ppm Major and minor element composition of the Upper Crust of the Earth with selected trace element ratios as given by Rudnick and Gao 2004. Kemp & Hawkesworth 2004 Rudnick & Gao 2004
Upper Continental Crust 37 Rb 82           ppm Major and minor element composition of the Upper Crust of the Earth with selected trace element ratios as given by Rudnick and Gao 2004. Kemp & Hawkesworth 2004 Rudnick & Gao 2004
Upper Continental Crust   Rb/Ba 0.13             Major and minor element composition of the Upper Crust of the Earth with selected trace element ratios as given by Rudnick and Gao 2004. Kemp & Hawkesworth 2004 Rudnick & Gao 2004
Upper Continental Crust   Rb/Sr 0.25             Major and minor element composition of the Upper Crust of the Earth with selected trace element ratios as given by Rudnick and Gao 2004. Kemp & Hawkesworth 2004 Rudnick & Gao 2004
Upper Continental Crust 21 Sc 14           ppm Major and minor element composition of the Upper Crust of the Earth with selected trace element ratios as given by Rudnick and Gao 2004. Kemp & Hawkesworth 2004 Rudnick & Gao 2004
Upper Continental Crust 14 Si 66.6           wt% Major and minor element composition of the Upper Crust of the Earth with selected trace element ratios as given by Rudnick and Gao 2004. Kemp & Hawkesworth 2004 Rudnick & Gao 2004
Upper Continental Crust 62 Sm 4.7           ppm Major and minor element composition of the Upper Crust of the Earth with selected trace element ratios as given by Rudnick and Gao 2004. Kemp & Hawkesworth 2004 Rudnick & Gao 2004
Upper Continental Crust 38 Sr 320           ppm Major and minor element composition of the Upper Crust of the Earth with selected trace element ratios as given by Rudnick and Gao 2004. Kemp & Hawkesworth 2004 Rudnick & Gao 2004
Upper Continental Crust   Sr/Nd 11.85             Major and minor element composition of the Upper Crust of the Earth with selected trace element ratios as given by Rudnick and Gao 2004. Kemp & Hawkesworth 2004 Rudnick & Gao 2004
Upper Continental Crust 73 Ta 0.9           ppm Major and minor element composition of the Upper Crust of the Earth with selected trace element ratios as given by Rudnick and Gao 2004. Kemp & Hawkesworth 2004 Rudnick & Gao 2004
Upper Continental Crust 65 Tb 0.7           ppm Major and minor element composition of the Upper Crust of the Earth with selected trace element ratios as given by Rudnick and Gao 2004. Kemp & Hawkesworth 2004 Rudnick & Gao 2004
Upper Continental Crust 90 Th 10.5           ppm Major and minor element composition of the Upper Crust of the Earth with selected trace element ratios as given by Rudnick and Gao 2004. Kemp & Hawkesworth 2004 Rudnick & Gao 2004
Upper Continental Crust 22 Ti 0.64           wt% Major and minor element composition of the Upper Crust of the Earth with selected trace element ratios as given by Rudnick and Gao 2004. Kemp & Hawkesworth 2004 Rudnick & Gao 2004
Upper Continental Crust 69 Tm 0.3           ppm Major and minor element composition of the Upper Crust of the Earth with selected trace element ratios as given by Rudnick and Gao 2004. Kemp & Hawkesworth 2004 Rudnick & Gao 2004
Upper Continental Crust 92 U 2.7           ppm Major and minor element composition of the Upper Crust of the Earth with selected trace element ratios as given by Rudnick and Gao 2004. Kemp & Hawkesworth 2004 Rudnick & Gao 2004
Upper Continental Crust 23 V 97           ppm Major and minor element composition of the Upper Crust of the Earth with selected trace element ratios as given by Rudnick and Gao 2004. Kemp & Hawkesworth 2004 Rudnick & Gao 2004
Upper Continental Crust 39 Y 21           ppm Major and minor element composition of the Upper Crust of the Earth with selected trace element ratios as given by Rudnick and Gao 2004. Kemp & Hawkesworth 2004 Rudnick & Gao 2004
Upper Continental Crust 70 Yb 2           ppm Major and minor element composition of the Upper Crust of the Earth with selected trace element ratios as given by Rudnick and Gao 2004. Kemp & Hawkesworth 2004 Rudnick & Gao 2004
Upper Continental Crust 30 Zn 67           ppm Major and minor element composition of the Upper Crust of the Earth with selected trace element ratios as given by Rudnick and Gao 2004. Kemp & Hawkesworth 2004 Rudnick & Gao 2004
Upper Continental Crust 40 Zr 193           ppm Major and minor element composition of the Upper Crust of the Earth with selected trace element ratios as given by Rudnick and Gao 2004. Kemp & Hawkesworth 2004 Rudnick & Gao 2004
Upper Continental Crust 55 Cs 7.3   0.29       ppm Revised upper continental crust (UCC) value calculated from the ratios as reported in Table 4 using Al2O3 = 15.2% and Rb = 122 ppm from the Taylor & McLennan (1985) estimate. Uncertainties are calculated from the standard deviations of the mean ratios in Table 4. Plank & Langmuir 1998
Upper Continental Crust 41 Nb 13.7   0.92       ppm Revised upper continental crust (UCC) value calculated from the ratios as reported in Table 4 using Al2O3 = 15.2% and Rb = 122 ppm from the Taylor & McLennan (1985) estimate. Uncertainties are calculated from the standard deviations of the mean ratios in Table 4. Plank & Langmuir 1998
Upper Continental Crust 73 Ta 0.96   0.12       ppm Revised upper continental crust (UCC) value calculated from the ratios as reported in Table 4 using Al2O3 = 15.2% and Rb = 122 ppm from the Taylor & McLennan (1985) estimate. Uncertainties are calculated from the standard deviations of the mean ratios in Table 4. Plank & Langmuir 1998
Upper Continental Crust 22 Ti 0.76   0.043       wt%ox Revised upper continental crust (UCC) value calculated from the ratios as reported in Table 4 using Al2O3 = 15.2% and Rb = 122 ppm from the Taylor & McLennan (1985) estimate. Uncertainties are calculated from the standard deviations of the mean ratios in Table 4. Plank & Langmuir 1998
Upper Continental Crust   Eu/Eu* 0.66             Rudnick & Fountain 1995
Upper Continental Crust   K/Rb 250             Rudnick & Fountain 1995
Upper Continental Crust   K/U 10             Rudnick & Fountain 1995
Upper Continental Crust   La/Nb 1.2             Rudnick & Fountain 1995
Upper Continental Crust   Rb/Cs 20             Rudnick & Fountain 1995
Upper Continental Crust   Rb/Sr 0.32             Rudnick & Fountain 1995
Upper Continental Crust   Sm/Nd 0.17             Rudnick & Fountain 1995
Upper Continental Crust   Sr/Nd 13             Rudnick & Fountain 1995
Upper Continental Crust   Th/U 3.8             Rudnick & Fountain 1995
Upper Continental Crust   U/Pb 0.14             Rudnick & Fountain 1995
Upper Continental Crust   Zr/Hf 33             Rudnick & Fountain 1995
Upper Continental Crust 47 Ag 55           ng/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Gao et al. 1998 and represent averages from surface exposures. Rudnick & Gao 2004 Gao et al. 1998
Upper Continental Crust 47 Ag 53   3       ng/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text








Upper Continental Crust 47 Ag 55           ng/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Wedepohl 1995 and represent a previous estimate. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 47 Ag 50           ng/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Taylor and McLennan 1985 & 1995 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Taylor & McLennan 1985
Taylor & McLennan 1995
Upper Continental Crust 47 Ag 53           ng/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 13 Al 15.14           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Condie 1993. Rudnick & Gao 2004 Condie 1993
Upper Continental Crust 13 Al 15.4   0.75       wt% Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text









Upper Continental Crust 13 Al 15.4           wt% Reccomended values for major element composition of the Upper Continental Crust as given in wt.% from Rudnick and Gao 2004. Rudnick & Gao 2004
Upper Continental Crust 13 Al 15.05           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Shaw et al. 1967. Rudnick & Gao 2004 Shaw et al. 1967
Upper Continental Crust 13 Al 16.63           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Goldschmidt 1933. Rudnick & Gao 2004 Goldschmidt 1933
Upper Continental Crust 13 Al 15.53           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Borodin 1998. Rudnick & Gao 2004 Borodin 1998
Upper Continental Crust 13 Al 15.84           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Ronov and Yaroshevskiy 1976. Rudnick & Gao 2004 Ronov & Yaroshevskiy 1976
Upper Continental Crust 13 Al 15.27           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Clarke 1889. Rudnick & Gao 2004 Clarke 1889
Upper Continental Crust 13 Al 14.17           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Gao et al. 1998a. Rudnick & Gao 2004 Gao et al. 1998
Upper Continental Crust 13 Al 15.05           wt% Major element composition of the Upper Continental Crust as given in wt.% using derivative compositions of data from Wedepohl 1995. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 13 Al 15.17           wt% Major element composition of the Upper Continental Crust as given in wt.% using derivative compositions of data from Taylor and McLennan 1985.Major element composition of the Upper Continental Crust as given in wt.% from derivative compositions of Taylor and McLennan 1985. Rudnick & Gao 2004 Taylor & McLennan 1985
Upper Continental Crust 13 Al 16.1           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Fahrig and Eade 1968. Rudnick & Gao 2004 Fahrig & Eade 1968
Upper Continental Crust 13 Al 15.65           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Clarke & Washington 1924. Rudnick & Gao 2004 Clarke & Washington 1924
Upper Continental Crust 33 As 4.8           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 33 As 1.5           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Taylor and McLennan 1985 & 1995 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Taylor & McLennan 1985
Taylor & McLennan 1995
Upper Continental Crust 33 As 2           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Wedepohl 1995 and represent a previous estimate. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 33 As 4.8   0.5       µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text










Upper Continental Crust 33 As 4.4           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Gao et al. 1998 and represent averages from surface exposures. Rudnick & Gao 2004 Gao et al. 1998
Upper Continental Crust 33 As 5.1           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Sims et al. 1990 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Sims et al. 1990
Upper Continental Crust 79 Au 1.5           ng/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 79 Au 1.81           ng/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Shaw et al. 1967 & 1976 and represent averages from surface exposures. Rudnick & Gao 2004 Shaw et al. 1967
Shaw et al. 1976
Upper Continental Crust 79 Au 1.5   0.4       ng/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text








Upper Continental Crust 79 Au 1.24           ng/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Gao et al. 1998 and represent averages from surface exposures. Rudnick & Gao 2004 Gao et al. 1998
Upper Continental Crust 79 Au 1.8           ng/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Taylor and McLennan 1985 & 1995 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Taylor & McLennan 1985
Taylor & McLennan 1995
Upper Continental Crust 5 B 15           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Taylor and McLennan 1985 & 1995 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Taylor & McLennan 1985
Taylor & McLennan 1995
Upper Continental Crust 5 B 17           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Wedepohl 1995 and represent a previous estimate. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 5 B 9.2           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Shaw et al. 1967 & 1976 and represent averages from surface exposures. Rudnick & Gao 2004 Shaw et al. 1967
Shaw et al. 1976
Upper Continental Crust 5 B 28           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Gao et al. 1998 and represent averages from surface exposures. Rudnick & Gao 2004 Gao et al. 1998
Upper Continental Crust 5 B 17           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 5 B 17   8       µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text








Upper Continental Crust 56 Ba 730           µg/g Estimates of trace element composition of the Upper Continental Crust. These values are taken from Eade and Fahrig 1973 and represent averages from surface exposures. Rudnick & Gao 2004 Eade and Fahrig 1973
Upper Continental Crust 56 Ba 624           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 56 Ba 550           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Taylor and McLennan 1985 & 1995 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Taylor & McLennan 1985
Taylor & McLennan 1995
Upper Continental Crust 56 Ba 628   83       µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text









Upper Continental Crust 56 Ba 1070           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Shaw et al. 1967 & 1976 and represent averages from surface exposures. Rudnick & Gao 2004 Shaw et al. 1967
Shaw et al. 1976
Upper Continental Crust 56 Ba 668           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Wedepohl 1995 and represent a previous estimate. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 56 Ba 633           µg/g Estimates of trace element composition of the Upper Continental Crust. These values are taken from Condie 1993 and represent averages from surface exposures. Rudnick & Gao 2004 Condie 1993
Upper Continental Crust 56 Ba 678           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Gao et al. 1998 and represent averages from surface exposures. Rudnick & Gao 2004 Gao et al. 1998
Upper Continental Crust 4 Be 2.1   0.9       µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text








Upper Continental Crust 4 Be 1.3           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Shaw et al. 1967 & 1976 and represent averages from surface exposures. Rudnick & Gao 2004 Shaw et al. 1967
Shaw et al. 1976
Upper Continental Crust 4 Be 1.95           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Gao et al. 1998 and represent averages from surface exposures. Rudnick & Gao 2004 Gao et al. 1998
Upper Continental Crust 4 Be 3           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Taylor and McLennan 1985 & 1995 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Taylor & McLennan 1985
Taylor & McLennan 1995
Upper Continental Crust 4 Be 3.1           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Wedepohl 1995 and represent a previous estimate. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 4 Be 2.1           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 83 Bi 0.123           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Wedepohl 1995 and represent a previous estimate. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 83 Bi 0.23           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Gao et al. 1998 and represent averages from surface exposures. Rudnick & Gao 2004 Gao et al. 1998
Upper Continental Crust 83 Bi 0.035           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Shaw et al. 1967 & 1976 and represent averages from surface exposures. Rudnick & Gao 2004 Shaw et al. 1967
Shaw et al. 1976
Upper Continental Crust 83 Bi 0.13           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Taylor and McLennan 1985 & 1995 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Taylor & McLennan 1985
Taylor & McLennan 1995
Upper Continental Crust 83 Bi 0.16   0.06       µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text









Upper Continental Crust 83 Bi 0.16           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 35 Br 1.6           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Wedepohl 1995 and represent a previous estimate. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 35 Br 1.6           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 35 Br 1.6           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text
Upper Continental Crust 20 Ca 3.64           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Condie 1993. Rudnick & Gao 2004 Condie 1993
Upper Continental Crust 20 Ca 3.59           wt% Reccomended values for major element composition of the Upper Continental Crust as given in wt.% from Rudnick and Gao 2004. Rudnick & Gao 2004
Upper Continental Crust 20 Ca 4.24           wt% Major element composition of the Upper Continental Crust as given in wt.% using derivative compositions of data from Wedepohl 1995. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 20 Ca 3.5           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Borodin 1998. Rudnick & Gao 2004 Borodin 1998
Upper Continental Crust 20 Ca 3.4           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Fahrig and Eade 1968. Rudnick & Gao 2004 Fahrig & Eade 1968
Upper Continental Crust 20 Ca 4.19           wt% Major element composition of the Upper Continental Crust as given in wt.% using derivative compositions of data from Taylor and McLennan 1985.Major element composition of the Upper Continental Crust as given in wt.% from derivative compositions of Taylor and McLennan 1985. Rudnick & Gao 2004 Taylor & McLennan 1985
Upper Continental Crust 20 Ca 3.59   0.2       wt% Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text









Upper Continental Crust 20 Ca 4.24           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Shaw et al. 1967. Rudnick & Gao 2004 Shaw et al. 1967
Upper Continental Crust 20 Ca 3.23           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Goldschmidt 1933. Rudnick & Gao 2004 Goldschmidt 1933
Upper Continental Crust 20 Ca 3.91           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Ronov and Yaroshevskiy 1976. Rudnick & Gao 2004 Ronov & Yaroshevskiy 1976
Upper Continental Crust 20 Ca 5.45           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Clarke 1889. Rudnick & Gao 2004 Clarke 1889
Upper Continental Crust 20 Ca 5.18           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Clarke & Washington 1924. Rudnick & Gao 2004 Clarke & Washington 1924
Upper Continental Crust 20 Ca 3.44           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Gao et al. 1998a. Rudnick & Gao 2004 Gao et al. 1998
Upper Continental Crust 48 Cd 0.079           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Gao et al. 1998 and represent averages from surface exposures. Rudnick & Gao 2004 Gao et al. 1998
Upper Continental Crust 48 Cd 0.102           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Wedepohl 1995 and represent a previous estimate. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 48 Cd 0.09           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 48 Cd 0.098           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Taylor and McLennan 1985 & 1995 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Taylor & McLennan 1985
Taylor & McLennan 1995
Upper Continental Crust 48 Cd 0.075           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Shaw et al. 1967 & 1976 and represent averages from surface exposures. Rudnick & Gao 2004 Shaw et al. 1967
Shaw et al. 1976
Upper Continental Crust 48 Cd 0.09   0.01       µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text








Upper Continental Crust 58 Ce 65.7           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Wedepohl 1995 and represent a previous estimate. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 58 Ce 64           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Taylor and McLennan 1985 & 1995 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Taylor & McLennan 1985
Taylor & McLennan 1995
Upper Continental Crust 58 Ce 65.6           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Shaw et al. 1967 & 1976 and represent averages from surface exposures. Rudnick & Gao 2004 Shaw et al. 1967
Shaw et al. 1976
Upper Continental Crust 58 Ce 63           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 58 Ce 66.4           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Gao et al. 1998 and represent averages from surface exposures. Rudnick & Gao 2004 Gao et al. 1998
Upper Continental Crust 58 Ce 57.5           µg/g Estimates of trace element composition of the Upper Continental Crust. These values are taken from Condie 1993 and represent averages from surface exposures. Rudnick & Gao 2004 Condie 1993
Upper Continental Crust 58 Ce 63   4       µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text








Upper Continental Crust 17 Cl 100           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Shaw et al. 1967 & 1976 and represent averages from surface exposures. Rudnick & Gao 2004 Shaw et al. 1967
Shaw et al. 1976
Upper Continental Crust 17 Cl 370           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 17 Cl 370   382       µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text








Upper Continental Crust 17 Cl 640           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Wedepohl 1995 and represent a previous estimate. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 17 Cl 142           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Gao et al. 1998 and represent averages from surface exposures. Rudnick & Gao 2004 Gao et al. 1998
Upper Continental Crust 27 Co 12           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Shaw et al. 1967 & 1976 and represent averages from surface exposures. Rudnick & Gao 2004 Shaw et al. 1967
Shaw et al. 1976
Upper Continental Crust 27 Co 12           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Wedepohl 1995 and represent a previous estimate. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 27 Co 17.3           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 27 Co 17           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Taylor and McLennan 1985 & 1995 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Taylor & McLennan 1985
Taylor & McLennan 1995
Upper Continental Crust 27 Co 17.3   0.6       µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text










Upper Continental Crust 27 Co 17           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Gao et al. 1998 and represent averages from surface exposures. Rudnick & Gao 2004 Gao et al. 1998
Upper Continental Crust 27 Co 18           µg/g Estimates of trace element composition of the Upper Continental Crust. These values are taken from Condie 1993 and represent averages from surface exposures. Rudnick & Gao 2004 Condie 1993
Upper Continental Crust 24 Cr 92   17       µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text










Upper Continental Crust 24 Cr 92           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 24 Cr 35           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Shaw et al. 1967 & 1976 and represent averages from surface exposures. Rudnick & Gao 2004 Shaw et al. 1967
Shaw et al. 1976
Upper Continental Crust 24 Cr 80           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Gao et al. 1998 and represent averages from surface exposures. Rudnick & Gao 2004 Gao et al. 1998
Upper Continental Crust 24 Cr 76           µg/g Estimates of trace element composition of the Upper Continental Crust. These values are taken from Eade and Fahrig 1973 and represent averages from surface exposures. Rudnick & Gao 2004 Eade and Fahrig 1973
Upper Continental Crust 24 Cr 85           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Taylor and McLennan 1985 & 1995 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Taylor & McLennan 1985
Taylor & McLennan 1995
Upper Continental Crust 24 Cr 35           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Wedepohl 1995 and represent a previous estimate. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 24 Cr 112           µg/g Estimates of trace element composition of the Upper Continental Crust. These values are taken from Condie 1993 and represent averages from surface exposures. Rudnick & Gao 2004 Condie 1993
Upper Continental Crust 55 Cs 5.8           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Wedepohl 1995 and represent a previous estimate. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 55 Cs 73           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Plank and Langmuir 1998 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Plank & Langmuir 1998
Upper Continental Crust 55 Cs 3.55           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Gao et al. 1998 and represent averages from surface exposures. Rudnick & Gao 2004 Gao et al. 1998
Upper Continental Crust 55 Cs 4.9   1.5       µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 55 Cs 4.6           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Taylor and McLennan 1985 & 1995 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Taylor & McLennan 1985
Taylor & McLennan 1995
Upper Continental Crust 55 Cs 4.9           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 29 Cu 26           µg/g Estimates of trace element composition of the Upper Continental Crust. These values are taken from Eade and Fahrig 1973 and represent averages from surface exposures. Rudnick & Gao 2004 Eade and Fahrig 1973
Upper Continental Crust 29 Cu 25           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Taylor and McLennan 1985 & 1995 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Taylor & McLennan 1985
Taylor & McLennan 1995
Upper Continental Crust 29 Cu 28   4       µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text









Upper Continental Crust 29 Cu 14           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Shaw et al. 1967 & 1976 and represent averages from surface exposures. Rudnick & Gao 2004 Shaw et al. 1967
Shaw et al. 1976
Upper Continental Crust 29 Cu 32           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Gao et al. 1998 and represent averages from surface exposures. Rudnick & Gao 2004 Gao et al. 1998
Upper Continental Crust 29 Cu 28           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 29 Cu 14           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Wedepohl 1995 and represent a previous estimate. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 66 Dy 3.5           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Taylor and McLennan 1985 & 1995 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Taylor & McLennan 1985
Taylor & McLennan 1995
Upper Continental Crust 66 Dy 3.9           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 66 Dy 3.9           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 66 Dy 2.9           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Wedepohl 1995 and represent a previous estimate. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 66 Dy 2.9           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Shaw et al. 1967 & 1976 and represent averages from surface exposures. Rudnick & Gao 2004 Shaw et al. 1967
Shaw et al. 1976
Upper Continental Crust 68 Er 2.3           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text








Upper Continental Crust 68 Er 2.3           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 68 Er 2.3           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Taylor and McLennan 1985 & 1995 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Taylor & McLennan 1985
Taylor & McLennan 1995
Upper Continental Crust 63 Eu 1   0.1       µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text








Upper Continental Crust 63 Eu 1           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 63 Eu 0.937           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Shaw et al. 1967 & 1976 and represent averages from surface exposures. Rudnick & Gao 2004 Shaw et al. 1967
Shaw et al. 1976
Upper Continental Crust 63 Eu 1.05           µg/g Estimates of trace element composition of the Upper Continental Crust. These values are taken from Condie 1993 and represent averages from surface exposures. Rudnick & Gao 2004 Condie 1993
Upper Continental Crust 63 Eu 0.95           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Wedepohl 1995 and represent a previous estimate. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 63 Eu 1.21           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Gao et al. 1998 and represent averages from surface exposures. Rudnick & Gao 2004 Gao et al. 1998
Upper Continental Crust 63 Eu 0.88           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Taylor and McLennan 1985 & 1995 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Taylor & McLennan 1985
Taylor & McLennan 1995
Upper Continental Crust 9 F 611           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Wedepohl 1995 and represent a previous estimate. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 9 F 500           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Shaw et al. 1967 & 1976 and represent averages from surface exposures. Rudnick & Gao 2004 Shaw et al. 1967
Shaw et al. 1976
Upper Continental Crust 9 F 561           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Gao et al. 1998 and represent averages from surface exposures. Rudnick & Gao 2004 Gao et al. 1998
Upper Continental Crust 9 F 557           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 9 F 557   56       µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text








Upper Continental Crust 26 Fe 7.26           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Clarke 1889. Rudnick & Gao 2004 Clarke 1889
Upper Continental Crust 26 Fe 6.7           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Clarke & Washington 1924. Rudnick & Gao 2004 Clarke & Washington 1924
Upper Continental Crust 26 Fe 4.09           wt% Major element composition of the Upper Continental Crust as given in wt.% using derivative compositions of data from Wedepohl 1995. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 26 Fe 5.04           wt% Reccomended values for major element composition of the Upper Continental Crust as given in wt.% from Rudnick and Gao 2004. Rudnick & Gao 2004
Upper Continental Crust 26 Fe 4.4           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Fahrig and Eade 1968. Rudnick & Gao 2004 Fahrig & Eade 1968
Upper Continental Crust 26 Fe 5.78           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Ronov and Yaroshevskiy 1976. Rudnick & Gao 2004 Ronov & Yaroshevskiy 1976
Upper Continental Crust 26 Fe 5.04   0.53       wt% Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text









Upper Continental Crust 26 Fe 4.09           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Shaw et al. 1967. Rudnick & Gao 2004 Shaw et al. 1967
Upper Continental Crust 26 Fe 4.76           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Condie 1993. Rudnick & Gao 2004 Condie 1993
Upper Continental Crust 26 Fe 5.33           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Gao et al. 1998a. Rudnick & Gao 2004 Gao et al. 1998
Upper Continental Crust 26 Fe 4.94           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Borodin 1998. Rudnick & Gao 2004 Borodin 1998
Upper Continental Crust 26 Fe 4.49           wt% Major element composition of the Upper Continental Crust as given in wt.% using derivative compositions of data from Taylor and McLennan 1985.Major element composition of the Upper Continental Crust as given in wt.% from derivative compositions of Taylor and McLennan 1985. Rudnick & Gao 2004 Taylor & McLennan 1985
Upper Continental Crust 26 Fe 6.99           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Goldschmidt 1933. Rudnick & Gao 2004 Goldschmidt 1933
Upper Continental Crust 31 Ga 17           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Taylor and McLennan 1985 & 1995 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Taylor & McLennan 1985
Taylor & McLennan 1995
Upper Continental Crust 31 Ga 14           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Wedepohl 1995 and represent a previous estimate. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 31 Ga 17.5           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 31 Ga 14           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Shaw et al. 1967 & 1976 and represent averages from surface exposures. Rudnick & Gao 2004 Shaw et al. 1967
Shaw et al. 1976
Upper Continental Crust 31 Ga 18           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Gao et al. 1998 and represent averages from surface exposures. Rudnick & Gao 2004 Gao et al. 1998
Upper Continental Crust 31 Ga 17.5   0.7       µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text









Upper Continental Crust 64 Gd 4           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 64 Gd 4   0.3       µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text








Upper Continental Crust 64 Gd 4.21           µg/g Estimates of trace element composition of the Upper Continental Crust. These values are taken from Condie 1993 and represent averages from surface exposures. Rudnick & Gao 2004 Condie 1993
Upper Continental Crust 64 Gd 3.8           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Taylor and McLennan 1985 & 1995 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Taylor & McLennan 1985
Taylor & McLennan 1995
Upper Continental Crust 64 Gd 2.8           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Wedepohl 1995 and represent a previous estimate. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 32 Ge 1.4           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Wedepohl 1995 and represent a previous estimate. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 32 Ge 1.6           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Taylor and McLennan 1985 & 1995 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Taylor & McLennan 1985
Taylor & McLennan 1995
Upper Continental Crust 32 Ge 1.4           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 32 Ge 1.4   0.1       µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text








Upper Continental Crust 32 Ge 1.34           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Gao et al. 1998 and represent averages from surface exposures. Rudnick & Gao 2004 Gao et al. 1998
Upper Continental Crust 72 Hf 5.12           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Gao et al. 1998 and represent averages from surface exposures. Rudnick & Gao 2004 Gao et al. 1998
Upper Continental Crust 72 Hf 4.3           µg/g Estimates of trace element composition of the Upper Continental Crust. These values are taken from Condie 1993 and represent averages from surface exposures. Rudnick & Gao 2004 Condie 1993
Upper Continental Crust 72 Hf 5.8           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Wedepohl 1995 and represent a previous estimate. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 72 Hf 5.3           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 72 Hf 5.3   0.7       µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text








Upper Continental Crust 72 Hf 5.8           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Shaw et al. 1967 & 1976 and represent averages from surface exposures. Rudnick & Gao 2004 Shaw et al. 1967
Shaw et al. 1976
Upper Continental Crust 72 Hf 5.8           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Taylor and McLennan 1985 & 1995 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Taylor & McLennan 1985
Taylor & McLennan 1995
Upper Continental Crust 80 Hg 0.05   0.04       µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text








Upper Continental Crust 80 Hg 0.056           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Wedepohl 1995 and represent a previous estimate. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 80 Hg 0.05           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 80 Hg 0.096           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Shaw et al. 1967 & 1976 and represent averages from surface exposures. Rudnick & Gao 2004 Shaw et al. 1967
Shaw et al. 1976
Upper Continental Crust 80 Hg 0.0123           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Gao et al. 1998 and represent averages from surface exposures. Rudnick & Gao 2004 Gao et al. 1998
Upper Continental Crust 67 Ho 0.8           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Taylor and McLennan 1985 & 1995 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Taylor & McLennan 1985
Taylor & McLennan 1995
Upper Continental Crust 67 Ho 0.62           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Wedepohl 1995 and represent a previous estimate. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 67 Ho 0.83           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 67 Ho 0.62           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Shaw et al. 1967 & 1976 and represent averages from surface exposures. Rudnick & Gao 2004 Shaw et al. 1967
Shaw et al. 1976
Upper Continental Crust 67 Ho 0.83           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 53 I 1.4           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Wedepohl 1995 and represent a previous estimate. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 53 I 1.4           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text
Upper Continental Crust 53 I 1.4           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 49 In 0.056           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 49 In 0.056   0.008       µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text








Upper Continental Crust 49 In 0.061           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Wedepohl 1995 and represent a previous estimate. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 49 In 0.05           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Taylor and McLennan 1985 & 1995 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Taylor & McLennan 1985
Taylor & McLennan 1995
Upper Continental Crust 77 Ir 0.022   0.007       ng/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text
Upper Continental Crust 77 Ir 0.022           ng/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 77 Ir 0.02           ng/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Taylor and McLennan 1985 & 1995 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Taylor & McLennan 1985
Taylor & McLennan 1995
Upper Continental Crust 77 Ir 0.022           ng/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Peucker-Ehrenbrink and Jahn 2001 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Peucker-Eherenbrink & Jahn 2001
Upper Continental Crust 77 Ir 0.02           ng/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Shaw et al. 1967 & 1976 and represent averages from surface exposures. Rudnick & Gao 2004 Shaw et al. 1967
Shaw et al. 1976
Upper Continental Crust 19 K 2.99           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Clarke 1889. Rudnick & Gao 2004 Clarke 1889
Upper Continental Crust 19 K 3.19           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Clarke & Washington 1924. Rudnick & Gao 2004 Clarke & Washington 1924
Upper Continental Crust 19 K 3.39           wt% Major element composition of the Upper Continental Crust as given in wt.% using derivative compositions of data from Taylor and McLennan 1985.Major element composition of the Upper Continental Crust as given in wt.% from derivative compositions of Taylor and McLennan 1985. Rudnick & Gao 2004 Taylor & McLennan 1985
Upper Continental Crust 19 K 3.19           wt% Major element composition of the Upper Continental Crust as given in wt.% using derivative compositions of data from Wedepohl 1995. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 19 K 2.8           wt% Reccomended values for major element composition of the Upper Continental Crust as given in wt.% from Rudnick and Gao 2004. Rudnick & Gao 2004
Upper Continental Crust 19 K 2.76           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Condie 1993. Rudnick & Gao 2004 Condie 1993
Upper Continental Crust 19 K 2.68           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Gao et al. 1998a. Rudnick & Gao 2004 Gao et al. 1998
Upper Continental Crust 19 K 3.01           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Borodin 1998. Rudnick & Gao 2004 Borodin 1998
Upper Continental Crust 19 K 2.8   0.23       wt% Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text









Upper Continental Crust 19 K 2.91           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Fahrig and Eade 1968. Rudnick & Gao 2004 Fahrig & Eade 1968
Upper Continental Crust 19 K 3.01           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Ronov and Yaroshevskiy 1976. Rudnick & Gao 2004 Ronov & Yaroshevskiy 1976
Upper Continental Crust 19 K 4.13           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Goldschmidt 1933. Rudnick & Gao 2004 Goldschmidt 1933
Upper Continental Crust 19 K 3.19           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Shaw et al. 1967. Rudnick & Gao 2004 Shaw et al. 1967
Upper Continental Crust 57 La 30           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Taylor and McLennan 1985 & 1995 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Taylor & McLennan 1985
Taylor & McLennan 1995
Upper Continental Crust 57 La 32.3           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Wedepohl 1995 and represent a previous estimate. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 57 La 28.4           µg/g Estimates of trace element composition of the Upper Continental Crust. These values are taken from Condie 1993 and represent averages from surface exposures. Rudnick & Gao 2004 Condie 1993
Upper Continental Crust 57 La 71           µg/g Estimates of trace element composition of the Upper Continental Crust. These values are taken from Eade and Fahrig 1973 and represent averages from surface exposures. Rudnick & Gao 2004 Eade and Fahrig 1973
Upper Continental Crust 57 La 34.8           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Gao et al. 1998 and represent averages from surface exposures. Rudnick & Gao 2004 Gao et al. 1998
Upper Continental Crust 57 La 31   3       µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text








Upper Continental Crust 57 La 32.3           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Shaw et al. 1967 & 1976 and represent averages from surface exposures. Rudnick & Gao 2004 Shaw et al. 1967
Shaw et al. 1976
Upper Continental Crust 57 La 31           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 3 Li 22           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Shaw et al. 1967 & 1976 and represent averages from surface exposures. Rudnick & Gao 2004 Shaw et al. 1967
Shaw et al. 1976
Upper Continental Crust 3 Li 20           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Gao et al. 1998 and represent averages from surface exposures. Rudnick & Gao 2004 Gao et al. 1998
Upper Continental Crust 3 Li 22           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Wedepohl 1995 and represent a previous estimate. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 3 Li 21           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 3 Li 20           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Taylor and McLennan 1985 & 1995 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Taylor & McLennan 1985
Taylor & McLennan 1995
Upper Continental Crust 3 Li 24   5       µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text









Upper Continental Crust 71 Lu 0.27           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Wedepohl 1995 and represent a previous estimate. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 71 Lu 0.31           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 71 Lu 0.233           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Shaw et al. 1967 & 1976 and represent averages from surface exposures. Rudnick & Gao 2004 Shaw et al. 1967
Shaw et al. 1976
Upper Continental Crust 71 Lu 0.31   0.05       µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text








Upper Continental Crust 71 Lu 0.32           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Taylor and McLennan 1985 & 1995 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Taylor & McLennan 1985
Taylor & McLennan 1995
Upper Continental Crust 71 Lu 0.35           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Gao et al. 1998 and represent averages from surface exposures. Rudnick & Gao 2004 Gao et al. 1998
Upper Continental Crust 71 Lu 0.32           µg/g Estimates of trace element composition of the Upper Continental Crust. These values are taken from Condie 1993 and represent averages from surface exposures. Rudnick & Gao 2004 Condie 1993
Upper Continental Crust 12 Mg 4.59           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Clarke 1889. Rudnick & Gao 2004 Clarke 1889
Upper Continental Crust 12 Mg 2.45           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Condie 1993. Rudnick & Gao 2004 Condie 1993
Upper Continental Crust 12 Mg 3.56           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Clarke & Washington 1924. Rudnick & Gao 2004 Clarke & Washington 1924
Upper Continental Crust 12 Mg 2.48           wt% Reccomended values for major element composition of the Upper Continental Crust as given in wt.% from Rudnick and Gao 2004. Rudnick & Gao 2004
Upper Continental Crust 12 Mg 2.62           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Gao et al. 1998a. Rudnick & Gao 2004 Gao et al. 1998
Upper Continental Crust 12 Mg 3.47           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Goldschmidt 1933. Rudnick & Gao 2004 Goldschmidt 1933
Upper Continental Crust 12 Mg 2.3           wt% Major element composition of the Upper Continental Crust as given in wt.% using derivative compositions of data from Wedepohl 1995. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 12 Mg 2.2           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Fahrig and Eade 1968. Rudnick & Gao 2004 Fahrig & Eade 1968
Upper Continental Crust 12 Mg 2.48   0.35       wt% Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text









Upper Continental Crust 12 Mg 2.2           wt% Major element composition of the Upper Continental Crust as given in wt.% using derivative compositions of data from Taylor and McLennan 1985.Major element composition of the Upper Continental Crust as given in wt.% from derivative compositions of Taylor and McLennan 1985. Rudnick & Gao 2004 Taylor & McLennan 1985
Upper Continental Crust 12 Mg 2.3           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Shaw et al. 1967. Rudnick & Gao 2004 Shaw et al. 1967
Upper Continental Crust 12 Mg 2.1           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Borodin 1998. Rudnick & Gao 2004 Borodin 1998
Upper Continental Crust 12 Mg 3.01           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Ronov and Yaroshevskiy 1976. Rudnick & Gao 2004 Ronov & Yaroshevskiy 1976
Upper Continental Crust   Mg# 48.1             Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Ronov and Yaroshevskiy 1976. Rudnick & Gao 2004 Ronov & Yaroshevskiy 1976
Upper Continental Crust   Mg# 46.7             Reccomended values for major element composition of the Upper Continental Crust as given in wt.% from Rudnick and Gao 2004. Rudnick & Gao 2004
Upper Continental Crust   Mg# 50.1             Major element composition of the Upper Continental Crust as given in wt.% using derivative compositions of data from Wedepohl 1995. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust   Mg# 46.6             Major element composition of the Upper Continental Crust as given in wt.% using derivative compositions of data from Taylor and McLennan 1985.Major element composition of the Upper Continental Crust as given in wt.% from derivative compositions of Taylor and McLennan 1985. Rudnick & Gao 2004 Taylor & McLennan 1985
Upper Continental Crust   Mg# 48.7             Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Goldschmidt 1933. Rudnick & Gao 2004 Goldschmidt 1933
Upper Continental Crust   Mg# 53             Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Clarke & Washington 1924. Rudnick & Gao 2004 Clarke & Washington 1924
Upper Continental Crust   Mg# 50.1             Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Shaw et al. 1967. Rudnick & Gao 2004 Shaw et al. 1967
Upper Continental Crust   Mg# 46.9             Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Goldschmidt 1933. Rudnick & Gao 2004 Goldschmidt 1933
Upper Continental Crust   Mg# 47.4             Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Fahrig and Eade 1968. Rudnick & Gao 2004 Fahrig & Eade 1968
Upper Continental Crust   Mg# 4             Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Borodin 1998. Rudnick & Gao 2004 Borodin 1998
Upper Continental Crust   Mg# 46.7             Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Gao et al. 1998a. Rudnick & Gao 2004 Gao et al. 1998
Upper Continental Crust   Mg# 47.9             Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Condie 1993. Rudnick & Gao 2004 Condie 1993
Upper Continental Crust 25 Mn 0.07           wt% Major element composition of the Upper Continental Crust as given in wt.% using derivative compositions of data from Wedepohl 1995. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 25 Mn 0.07           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Shaw et al. 1967. Rudnick & Gao 2004 Shaw et al. 1967
Upper Continental Crust 25 Mn 0.12           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Clarke & Washington 1924. Rudnick & Gao 2004 Clarke & Washington 1924
Upper Continental Crust 25 Mn 0.1           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Gao et al. 1998a. Rudnick & Gao 2004 Gao et al. 1998
Upper Continental Crust 25 Mn 0.1           wt% Reccomended values for major element composition of the Upper Continental Crust as given in wt.% from Rudnick and Gao 2004. Rudnick & Gao 2004
Upper Continental Crust 25 Mn 0           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Borodin 1998. Rudnick & Gao 2004 Borodin 1998
Upper Continental Crust 25 Mn 0.12           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Goldschmidt 1933. Rudnick & Gao 2004 Goldschmidt 1933
Upper Continental Crust 25 Mn 0.07           wt% Major element composition of the Upper Continental Crust as given in wt.% using derivative compositions of data from Taylor and McLennan 1985.Major element composition of the Upper Continental Crust as given in wt.% from derivative compositions of Taylor and McLennan 1985. Rudnick & Gao 2004 Taylor & McLennan 1985
Upper Continental Crust 25 Mn 0.1   0.01       wt% Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text









Upper Continental Crust 25 Mn 0.08           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Fahrig and Eade 1968. Rudnick & Gao 2004 Fahrig & Eade 1968
Upper Continental Crust 25 Mn 0.1           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Clarke 1889. Rudnick & Gao 2004 Clarke 1889
Upper Continental Crust 25 Mn 0.1           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Ronov and Yaroshevskiy 1976. Rudnick & Gao 2004 Ronov & Yaroshevskiy 1976
Upper Continental Crust 42 Mo 1.1           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 42 Mo 1.2           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Sims et al. 1990 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Sims et al. 1990
Upper Continental Crust 42 Mo 1.4           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Wedepohl 1995 and represent a previous estimate. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 42 Mo 1.5           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Taylor and McLennan 1985 & 1995 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Taylor & McLennan 1985
Taylor & McLennan 1995
Upper Continental Crust 42 Mo 0.78           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Gao et al. 1998 and represent averages from surface exposures. Rudnick & Gao 2004 Gao et al. 1998
Upper Continental Crust 42 Mo 1.1   0.3       µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text









Upper Continental Crust 7 N 83           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Wedepohl 1995 and represent a previous estimate. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 7 N 83           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text
Upper Continental Crust 7 N 83           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 11 Na 3.9           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Fahrig and Eade 1968. Rudnick & Gao 2004 Fahrig & Eade 1968
Upper Continental Crust 11 Na 2.86           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Gao et al. 1998a. Rudnick & Gao 2004 Gao et al. 1998
Upper Continental Crust 11 Na 3.56           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Shaw et al. 1967. Rudnick & Gao 2004 Shaw et al. 1967
Upper Continental Crust 11 Na 3.27           wt% Reccomended values for major element composition of the Upper Continental Crust as given in wt.% from Rudnick and Gao 2004. Rudnick & Gao 2004
Upper Continental Crust 11 Na 3.56           wt% Major element composition of the Upper Continental Crust as given in wt.% using derivative compositions of data from Wedepohl 1995. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 11 Na 3.21           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Borodin 1998. Rudnick & Gao 2004 Borodin 1998
Upper Continental Crust 11 Na 3.92           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Clarke & Washington 1924. Rudnick & Gao 2004 Clarke & Washington 1924
Upper Continental Crust 11 Na 3.29           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Clarke 1889. Rudnick & Gao 2004 Clarke 1889
Upper Continental Crust 11 Na 3.89           wt% Major element composition of the Upper Continental Crust as given in wt.% using derivative compositions of data from Taylor and McLennan 1985.Major element composition of the Upper Continental Crust as given in wt.% from derivative compositions of Taylor and McLennan 1985. Rudnick & Gao 2004 Taylor & McLennan 1985
Upper Continental Crust 11 Na 3.55           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Condie 1993. Rudnick & Gao 2004 Condie 1993
Upper Continental Crust 11 Na 2.81           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Ronov and Yaroshevskiy 1976. Rudnick & Gao 2004 Ronov & Yaroshevskiy 1976
Upper Continental Crust 11 Na 2.15           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Goldschmidt 1933. Rudnick & Gao 2004 Goldschmidt 1933
Upper Continental Crust 11 Na 3.27   0.48       wt% Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text









Upper Continental Crust 41 Nb 12           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Taylor and McLennan 1985 & 1995 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Taylor & McLennan 1985
Taylor & McLennan 1995
Upper Continental Crust 41 Nb 12           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Gao et al. 1998 and represent averages from surface exposures. Rudnick & Gao 2004 Gao et al. 1998
Upper Continental Crust 41 Nb 12   1       µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text









Upper Continental Crust 41 Nb 9.8           µg/g Estimates of trace element composition of the Upper Continental Crust. These values are taken from Condie 1993 and represent averages from surface exposures. Rudnick & Gao 2004 Condie 1993
Upper Continental Crust 41 Nb 26           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Wedepohl 1995 and represent a previous estimate. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 41 Nb 12           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 41 Nb 13.7           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Plank and Langmuir 1998 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Plank & Langmuir 1998
Upper Continental Crust 41 Nb 26           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Shaw et al. 1967 & 1976 and represent averages from surface exposures. Rudnick & Gao 2004 Shaw et al. 1967
Shaw et al. 1976
Upper Continental Crust 60 Nd 27           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 60 Nd 25.9           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Shaw et al. 1967 & 1976 and represent averages from surface exposures. Rudnick & Gao 2004 Shaw et al. 1967
Shaw et al. 1976
Upper Continental Crust 60 Nd 27   2       µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text








Upper Continental Crust 60 Nd 30.4           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Gao et al. 1998 and represent averages from surface exposures. Rudnick & Gao 2004 Gao et al. 1998
Upper Continental Crust 60 Nd 26           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Taylor and McLennan 1985 & 1995 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Taylor & McLennan 1985
Taylor & McLennan 1995
Upper Continental Crust 60 Nd 25.6           µg/g Estimates of trace element composition of the Upper Continental Crust. These values are taken from Condie 1993 and represent averages from surface exposures. Rudnick & Gao 2004 Condie 1993
Upper Continental Crust 28 Ni 47           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 28 Ni 19           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Shaw et al. 1967 & 1976 and represent averages from surface exposures. Rudnick & Gao 2004 Shaw et al. 1967
Shaw et al. 1976
Upper Continental Crust 28 Ni 38           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Gao et al. 1998 and represent averages from surface exposures. Rudnick & Gao 2004 Gao et al. 1998
Upper Continental Crust 28 Ni 60           µg/g Estimates of trace element composition of the Upper Continental Crust. These values are taken from Condie 1993 and represent averages from surface exposures. Rudnick & Gao 2004 Condie 1993
Upper Continental Crust 28 Ni 19           µg/g Estimates of trace element composition of the Upper Continental Crust. These values are taken from Eade and Fahrig 1973 and represent averages from surface exposures. Rudnick & Gao 2004 Eade and Fahrig 1973
Upper Continental Crust 28 Ni 44           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Taylor and McLennan 1985 & 1995 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Taylor & McLennan 1985
Taylor & McLennan 1995
Upper Continental Crust 28 Ni 19           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Wedepohl 1995 and represent a previous estimate. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 28 Ni 47   11       µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text










Upper Continental Crust 76 Os 0.031           ng/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Peucker-Ehrenbrink and Jahn 2001 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Peucker-Eherenbrink & Jahn 2001
Upper Continental Crust 76 Os 0.031           ng/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 76 Os 0.031   0.009       ng/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text
Upper Continental Crust 76 Os 0.05           ng/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Taylor and McLennan 1985 & 1995 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Taylor & McLennan 1985
Taylor & McLennan 1995
Upper Continental Crust 15 P 0.23             Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Clarke 1889. Rudnick & Gao 2004 Clarke 1889
Upper Continental Crust 15 P 0.31             Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Clarke & Washington 1924. Rudnick & Gao 2004 Clarke & Washington 1924
Upper Continental Crust 15 P 0.2           wt% Major element composition of the Upper Continental Crust as given in wt.% using derivative compositions of data from Taylor and McLennan 1985.Major element composition of the Upper Continental Crust as given in wt.% from derivative compositions of Taylor and McLennan 1985. Rudnick & Gao 2004 Taylor & McLennan 1985
Upper Continental Crust 15 P 0.15           wt% Major element composition of the Upper Continental Crust as given in wt.% using derivative compositions of data from Wedepohl 1995. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 15 P 0.15           wt% Reccomended values for major element composition of the Upper Continental Crust as given in wt.% from Rudnick and Gao 2004. Rudnick & Gao 2004
Upper Continental Crust 15 P 0.12           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Condie 1993. Rudnick & Gao 2004 Condie 1993
Upper Continental Crust 15 P 0.16           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Gao et al. 1998a. Rudnick & Gao 2004 Gao et al. 1998
Upper Continental Crust 15 P 0           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Borodin 1998. Rudnick & Gao 2004 Borodin 1998
Upper Continental Crust 15 P 0.15   0.02       wt% Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text









Upper Continental Crust 15 P 0.16           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Fahrig and Eade 1968. Rudnick & Gao 2004 Fahrig & Eade 1968
Upper Continental Crust 15 P 0.16           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Ronov and Yaroshevskiy 1976. Rudnick & Gao 2004 Ronov & Yaroshevskiy 1976
Upper Continental Crust 15 P 0.23           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Goldschmidt 1933. Rudnick & Gao 2004 Goldschmidt 1933
Upper Continental Crust 15 P 0.15           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Shaw et al. 1967. Rudnick & Gao 2004 Shaw et al. 1967
Upper Continental Crust 82 Pb 17   0.5       µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text








Upper Continental Crust 82 Pb 17           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Shaw et al. 1967 & 1976 and represent averages from surface exposures. Rudnick & Gao 2004 Shaw et al. 1967
Shaw et al. 1976
Upper Continental Crust 82 Pb 18           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Gao et al. 1998 and represent averages from surface exposures. Rudnick & Gao 2004 Gao et al. 1998
Upper Continental Crust 82 Pb 17           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 82 Pb 17           µg/g Estimates of trace element composition of the Upper Continental Crust. These values are taken from Condie 1993 and represent averages from surface exposures. Rudnick & Gao 2004 Condie 1993
Upper Continental Crust 82 Pb 17           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Wedepohl 1995 and represent a previous estimate. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 82 Pb 18           µg/g Estimates of trace element composition of the Upper Continental Crust. These values are taken from Eade and Fahrig 1973 and represent averages from surface exposures. Rudnick & Gao 2004 Eade and Fahrig 1973
Upper Continental Crust 82 Pb 17           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Taylor and McLennan 1985 & 1995 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Taylor & McLennan 1985
Taylor & McLennan 1995
Upper Continental Crust 46 Pd 0.5           ng/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Taylor and McLennan 1985 & 1995 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Taylor & McLennan 1985
Taylor & McLennan 1995
Upper Continental Crust 46 Pd 0.52           ng/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Peucker-Ehrenbrink and Jahn 2001 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Peucker-Eherenbrink & Jahn 2001
Upper Continental Crust 46 Pd 1.46           ng/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Gao et al. 1998 and represent averages from surface exposures. Rudnick & Gao 2004 Gao et al. 1998
Upper Continental Crust 46 Pd 0.52           ng/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 46 Pd 0.52   0.02       ng/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text
Upper Continental Crust 59 Pr 7.1           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text








Upper Continental Crust 59 Pr 6.3           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Wedepohl 1995 and represent a previous estimate. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 59 Pr 7.1           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 59 Pr 7.1           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Taylor and McLennan 1985 & 1995 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Taylor & McLennan 1985
Taylor & McLennan 1995
Upper Continental Crust 78 Pt 0.5           ng/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 78 Pt 0.51           ng/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Peucker-Ehrenbrink and Jahn 2001 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Peucker-Eherenbrink & Jahn 2001
Upper Continental Crust 78 Pt 0.5   0.5       ng/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text
Upper Continental Crust 37 Rb 110           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Wedepohl 1995 and represent a previous estimate. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 37 Rb 83           µg/g Estimates of trace element composition of the Upper Continental Crust. These values are taken from Condie 1993 and represent averages from surface exposures. Rudnick & Gao 2004 Condie 1993
Upper Continental Crust 37 Rb 84           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 37 Rb 110           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Shaw et al. 1967 & 1976 and represent averages from surface exposures. Rudnick & Gao 2004 Shaw et al. 1967
Shaw et al. 1976
Upper Continental Crust 37 Rb 84   17       µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 37 Rb 82           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Gao et al. 1998 and represent averages from surface exposures. Rudnick & Gao 2004 Gao et al. 1998
Upper Continental Crust 37 Rb 85           µg/g Estimates of trace element composition of the Upper Continental Crust. These values are taken from Eade and Fahrig 1973 and represent averages from surface exposures. Rudnick & Gao 2004 Eade and Fahrig 1973
Upper Continental Crust 37 Rb 112           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Taylor and McLennan 1985 & 1995 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Taylor & McLennan 1985
Taylor & McLennan 1995
Upper Continental Crust 75 Re 0.198           ng/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 75 Re 0.198           ng/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text
Upper Continental Crust 75 Re 0.4           ng/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Taylor and McLennan 1985 & 1995 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Taylor & McLennan 1985
Taylor & McLennan 1995
Upper Continental Crust 75 Re 0.198           ng/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Peucker-Ehrenbrink and Jahn 2001 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Peucker-Eherenbrink & Jahn 2001
Upper Continental Crust 44 Ru 0.34           ng/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 44 Ru 0.34   0.02       ng/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text
Upper Continental Crust 44 Ru 0.34           ng/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Peucker-Ehrenbrink and Jahn 2001 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Peucker-Eherenbrink & Jahn 2001
Upper Continental Crust 16 S 953           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Wedepohl 1995 and represent a previous estimate. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 16 S 309           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Gao et al. 1998 and represent averages from surface exposures. Rudnick & Gao 2004 Gao et al. 1998
Upper Continental Crust 16 S 62   33       µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text








Upper Continental Crust 16 S 600           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Shaw et al. 1967 & 1976 and represent averages from surface exposures. Rudnick & Gao 2004 Shaw et al. 1967
Shaw et al. 1976
Upper Continental Crust 16 S 621           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 51 Sb 0.31           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Wedepohl 1995 and represent a previous estimate. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 51 Sb 0.3           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Gao et al. 1998 and represent averages from surface exposures. Rudnick & Gao 2004 Gao et al. 1998
Upper Continental Crust 51 Sb 0.45           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Sims et al. 1990 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Sims et al. 1990
Upper Continental Crust 51 Sb 0.2           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Taylor and McLennan 1985 & 1995 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Taylor & McLennan 1985
Taylor & McLennan 1995
Upper Continental Crust 51 Sb 0.4   0.1       µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text










Upper Continental Crust 51 Sb 0.4           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 21 Sc 12           µg/g Estimates of trace element composition of the Upper Continental Crust. These values are taken from Eade and Fahrig 1973 and represent averages from surface exposures. Rudnick & Gao 2004 Eade and Fahrig 1973
Upper Continental Crust 21 Sc 7           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Wedepohl 1995 and represent a previous estimate. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 21 Sc 13.4           µg/g Estimates of trace element composition of the Upper Continental Crust. These values are taken from Condie 1993 and represent averages from surface exposures. Rudnick & Gao 2004 Condie 1993
Upper Continental Crust 21 Sc 14           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 21 Sc 14   0.9       µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text










Upper Continental Crust 21 Sc 15           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Gao et al. 1998 and represent averages from surface exposures. Rudnick & Gao 2004 Gao et al. 1998
Upper Continental Crust 21 Sc 13.6           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Taylor and McLennan 1985 & 1995 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Taylor & McLennan 1985
Taylor & McLennan 1995
Upper Continental Crust 21 Sc 7           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Shaw et al. 1967 & 1976 and represent averages from surface exposures. Rudnick & Gao 2004 Shaw et al. 1967
Shaw et al. 1976
Upper Continental Crust 34 Se 0.09   0.05       µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text








Upper Continental Crust 34 Se 0.09           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 34 Se 0.083           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Wedepohl 1995 and represent a previous estimate. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 34 Se 0.15           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Gao et al. 1998 and represent averages from surface exposures. Rudnick & Gao 2004 Gao et al. 1998
Upper Continental Crust 34 Se 0.05           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Taylor and McLennan 1985 & 1995 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Taylor & McLennan 1985
Taylor & McLennan 1995
Upper Continental Crust 14 Si 60.3           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Clarke & Washington 1924. Rudnick & Gao 2004 Clarke & Washington 1924
Upper Continental Crust 14 Si 60.2           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Clarke 1889. Rudnick & Gao 2004 Clarke 1889
Upper Continental Crust 14 Si 64.8           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Ronov and Yaroshevskiy 1976. Rudnick & Gao 2004 Ronov & Yaroshevskiy 1976
Upper Continental Crust 14 Si 66.2           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Fahrig and Eade 1968. Rudnick & Gao 2004 Fahrig & Eade 1968
Upper Continental Crust 14 Si 66.6   1.18       wt% Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text









Upper Continental Crust 14 Si 65.89           wt% Major element composition of the Upper Continental Crust as given in wt.% using derivative compositions of data from Taylor and McLennan 1985.Major element composition of the Upper Continental Crust as given in wt.% from derivative compositions of Taylor and McLennan 1985. Rudnick & Gao 2004 Taylor & McLennan 1985
Upper Continental Crust 14 Si 67.12           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Borodin 1998. Rudnick & Gao 2004 Borodin 1998
Upper Continental Crust 14 Si 67.97           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Gao et al. 1998a. Rudnick & Gao 2004 Gao et al. 1998
Upper Continental Crust 14 Si 67           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Condie 1993. Rudnick & Gao 2004 Condie 1993
Upper Continental Crust 14 Si 66.62           wt% Reccomended values for major element composition of the Upper Continental Crust as given in wt.% from Rudnick and Gao 2004. Rudnick & Gao 2004
Upper Continental Crust 14 Si 66.8           wt% Major element composition of the Upper Continental Crust as given in wt.% using derivative compositions of data from Wedepohl 1995. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 14 Si 66.8           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Shaw et al. 1967. Rudnick & Gao 2004 Shaw et al. 1967
Upper Continental Crust 14 Si 62.22           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Goldschmidt 1933. Rudnick & Gao 2004 Goldschmidt 1933
Upper Continental Crust 62 Sm 4.7   0.3       µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text








Upper Continental Crust 62 Sm 4.61           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Shaw et al. 1967 & 1976 and represent averages from surface exposures. Rudnick & Gao 2004 Shaw et al. 1967
Shaw et al. 1976
Upper Continental Crust 62 Sm 4.7           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 62 Sm 4.7           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Wedepohl 1995 and represent a previous estimate. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 62 Sm 5.09           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Gao et al. 1998 and represent averages from surface exposures. Rudnick & Gao 2004 Gao et al. 1998
Upper Continental Crust 62 Sm 4.5           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Taylor and McLennan 1985 & 1995 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Taylor & McLennan 1985
Taylor & McLennan 1995
Upper Continental Crust 62 Sm 4.59           µg/g Estimates of trace element composition of the Upper Continental Crust. These values are taken from Condie 1993 and represent averages from surface exposures. Rudnick & Gao 2004 Condie 1993
Upper Continental Crust 50 Sn 2.1   0.5       µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text










Upper Continental Crust 50 Sn 5.5           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Taylor and McLennan 1985 & 1995 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Taylor & McLennan 1985
Taylor & McLennan 1995
Upper Continental Crust 50 Sn 2.1           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 50 Sn 1.73           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Gao et al. 1998 and represent averages from surface exposures. Rudnick & Gao 2004 Gao et al. 1998
Upper Continental Crust 50 Sn 2.5           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Wedepohl 1995 and represent a previous estimate. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 38 Sr 350           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Taylor and McLennan 1985 & 1995 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Taylor & McLennan 1985
Taylor & McLennan 1995
Upper Continental Crust 38 Sr 380           µg/g Estimates of trace element composition of the Upper Continental Crust. These values are taken from Eade and Fahrig 1973 and represent averages from surface exposures. Rudnick & Gao 2004 Eade and Fahrig 1973
Upper Continental Crust 38 Sr 289           µg/g Estimates of trace element composition of the Upper Continental Crust. These values are taken from Condie 1993 and represent averages from surface exposures. Rudnick & Gao 2004 Condie 1993
Upper Continental Crust 38 Sr 316           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Shaw et al. 1967 & 1976 and represent averages from surface exposures. Rudnick & Gao 2004 Shaw et al. 1967
Shaw et al. 1976
Upper Continental Crust 38 Sr 320   46       µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text








Upper Continental Crust 38 Sr 266           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Gao et al. 1998 and represent averages from surface exposures. Rudnick & Gao 2004 Gao et al. 1998
Upper Continental Crust 38 Sr 320           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 38 Sr 316           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Wedepohl 1995 and represent a previous estimate. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 73 Ta 1.5           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Wedepohl 1995 and represent a previous estimate. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 73 Ta 0.79           µg/g Estimates of trace element composition of the Upper Continental Crust. These values are taken from Condie 1993 and represent averages from surface exposures. Rudnick & Gao 2004 Condie 1993
Upper Continental Crust 73 Ta 0.9           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 73 Ta 0.74           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Gao et al. 1998 and represent averages from surface exposures. Rudnick & Gao 2004 Gao et al. 1998
Upper Continental Crust 73 Ta 1           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Taylor and McLennan 1985 & 1995 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Taylor & McLennan 1985
Taylor & McLennan 1995
Upper Continental Crust 73 Ta 0.96           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Plank and Langmuir 1998 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Plank & Langmuir 1998
Upper Continental Crust 73 Ta 0.9   0.1       µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text









Upper Continental Crust 73 Ta 5.7           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Shaw et al. 1967 & 1976 and represent averages from surface exposures. Rudnick & Gao 2004 Shaw et al. 1967
Shaw et al. 1976
Upper Continental Crust 65 Tb 0.82           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Gao et al. 1998 and represent averages from surface exposures. Rudnick & Gao 2004 Gao et al. 1998
Upper Continental Crust 65 Tb 0.481           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Shaw et al. 1967 & 1976 and represent averages from surface exposures. Rudnick & Gao 2004 Shaw et al. 1967
Shaw et al. 1976
Upper Continental Crust 65 Tb 0.7   0.1       µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text








Upper Continental Crust 65 Tb 0.64           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Taylor and McLennan 1985 & 1995 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Taylor & McLennan 1985
Taylor & McLennan 1995
Upper Continental Crust 65 Tb 0.66           µg/g Estimates of trace element composition of the Upper Continental Crust. These values are taken from Condie 1993 and represent averages from surface exposures. Rudnick & Gao 2004 Condie 1993
Upper Continental Crust 65 Tb 0.7           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 65 Tb 0.5           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Wedepohl 1995 and represent a previous estimate. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 90 Th 8.6           µg/g Estimates of trace element composition of the Upper Continental Crust. These values are taken from Condie 1993 and represent averages from surface exposures. Rudnick & Gao 2004 Condie 1993
Upper Continental Crust 90 Th 10.8           µg/g Estimates of trace element composition of the Upper Continental Crust. These values are taken from Eade and Fahrig 1973 and represent averages from surface exposures. Rudnick & Gao 2004 Eade and Fahrig 1973
Upper Continental Crust 90 Th 10.3           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Wedepohl 1995 and represent a previous estimate. Rudnick & Gao 2004 Wedepohl 1995
Upper Continental Crust 90 Th 10.5   1       µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text

Upper Continental Crust 90 Th 10.3           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Shaw et al. 1967 & 1976 and represent averages from surface exposures. Rudnick & Gao 2004 Shaw et al. 1967
Shaw et al. 1976
Upper Continental Crust 90 Th 8.95           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Gao et al. 1998 and represent averages from surface exposures. Rudnick & Gao 2004 Gao et al. 1998
Upper Continental Crust 90 Th 10.7           µg/g Estimates of trace element compositions of the Upper Continental Crust. These values are taken from Taylor and McLennan 1985 & 1995 and represent estimates derived from sedimentary and loess data. Rudnick & Gao 2004 Taylor & McLennan 1985
Taylor & McLennan 1995
Upper Continental Crust 90 Th 10.5           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 22 Ti 0.55           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Ronov and Yaroshevskiy 1976. Rudnick & Gao 2004 Ronov & Yaroshevskiy 1976
Upper Continental Crust 22 Ti 0.64           wt% Reccomended values for major element composition of the Upper Continental Crust as given in wt.% from Rudnick and Gao 2004. Rudnick & Gao 2004
Upper Continental Crust 22 Ti 0.5           wt% Major element composition of the Upper Continental Crust as given in wt.% using derivative compositions of data from Taylor and McLennan 1985.Major element composition of the Upper Continental Crust as given in wt.% from derivative compositions of Taylor and McLennan 1985. Rudnick & Gao 2004 Taylor & McLennan 1985
Upper Continental Crust 22 Ti 0.9           µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004
Upper Continental Crust 22 Ti 0.67           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Gao et al. 1998a. Rudnick & Gao 2004 Gao et al. 1998
Upper Continental Crust 22 Ti 0.9   0.5       µg/g Recommended composition of the Upper Continental Crust as given by various sources which are listed in Table 1 and 2 of Rudnick and Gao 2004 as well as in the text. Rudnick & Gao 2004 see text








Upper Continental Crust 22 Ti 0.57           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Clarke 1889. Rudnick & Gao 2004 Clarke 1889
Upper Continental Crust 22 Ti 1.07           wt% Major element composition of the Upper Continental Crust as given in wt.% from either surface exposures or glacial clays. These values were first given by Clarke & Washington 1924. Rudnick & Gao 2004 Clarke & Washington 1924
Upper Continental Crust