GERM Reservoir Database
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GERM Database Search Results        
Reservoir Z Element Value Median SD Low High N Unit Info Reference Source(s)
Silty Mud 13 Al 15.34         16 wt%ox The hemi-pelagic clay analyses where averaged over 10 m intervals and then averaged down-unit. Plank & Langmuir 1998
Silty Mud 56 Ba 1571         16 ppm The hemi-pelagic clay analyses where averaged over 10 m intervals and then averaged down-unit. Plank & Langmuir 1998
Silty Mud 6 C 0         16 wt%ox The hemi-pelagic clay analyses where averaged over 10 m intervals and then averaged down-unit. Plank & Langmuir 1998
Silty Mud 20 Ca 1.4         16 wt%ox The hemi-pelagic clay analyses where averaged over 10 m intervals and then averaged down-unit. Plank & Langmuir 1998
Silty Mud 58 Ce 57.03         16 ppm The hemi-pelagic clay analyses where averaged over 10 m intervals and then averaged down-unit. Ce is calculated from the REE pattern in the Aleutian clastic turbidite. Plank & Langmuir 1998
Silty Mud 27 Co 26.4         16 ppm The hemi-pelagic clay analyses where averaged over 10 m intervals and then averaged down-unit. Plank & Langmuir 1998
Silty Mud 24 Cr 95.9         16 ppm The hemi-pelagic clay analyses where averaged over 10 m intervals and then averaged down-unit. Plank & Langmuir 1998
Silty Mud 55 Cs 3.69         16 ppm The hemi-pelagic clay analyses where averaged over 10 m intervals and then averaged down-unit. Cs is calculated from the continental ratio Cs/Rb = 0.065 because the Cr/Al2O3 and La/Al2O3 in the hemipelagic clay is typically continental. Plank & Langmuir 1998
Silty Mud 29 Cu 173.3         16 ppm The hemi-pelagic clay analyses where averaged over 10 m intervals and then averaged down-unit. Plank & Langmuir 1998
Silty Mud 66 Dy 5.17         16 ppm The hemi-pelagic clay analyses where averaged over 10 m intervals and then averaged down-unit. Dy is calculated from the REE pattern in the Aleutian clastic turbidite. Plank & Langmuir 1998
Silty Mud 68 Er 2.98         16 ppm The hemi-pelagic clay analyses where averaged over 10 m intervals and then averaged down-unit. Er is calculated from the REE pattern in the Aleutian clastic turbidite. Plank & Langmuir 1998
Silty Mud 63 Eu 1.46         16 ppm The hemi-pelagic clay analyses where averaged over 10 m intervals and then averaged down-unit. Eu is calculated from the REE pattern in the Aleutian clastic turbidite. Plank & Langmuir 1998
Silty Mud 26 Fe 8.28         16 wt%ox The hemi-pelagic clay analyses where averaged over 10 m intervals and then averaged down-unit. Plank & Langmuir 1998
Silty Mud 64 Gd 5.77         16 ppm The hemi-pelagic clay analyses where averaged over 10 m intervals and then averaged down-unit. Gd is calculated from the REE pattern in the Aleutian clastic turbidite. Plank & Langmuir 1998
Silty Mud 1 H 10         16 wt%ox The hemi-pelagic clay analyses where averaged over 10 m intervals and then averaged down-unit. Assumed 10% LOI. Plank & Langmuir 1998
Silty Mud 72 Hf 4.15         16 ppm The hemi-pelagic clay analyses where averaged over 10 m intervals and then averaged down-unit. Hf is calculated from Zr/Hf = 35. Plank & Langmuir 1998
Silty Mud 19 K 1.42         16 wt%ox The hemi-pelagic clay analyses where averaged over 10 m intervals and then averaged down-unit. Plank & Langmuir 1998
Silty Mud 57 La 27.69         16 ppm The hemi-pelagic clay analyses where averaged over 10 m intervals and then averaged down-unit. La is calculated from the continental ratio La/Sm = 5.6 because the Cr/Al2O3 and La/Al2O3 in the hemipelagic clay is typically continental. Plank & Langmuir 1998
Silty Mud 71 Lu 0.42         16 ppm The hemi-pelagic clay analyses where averaged over 10 m intervals and then averaged down-unit. Lu is calculated from the REE pattern in the Aleutian clastic turbidite. Plank & Langmuir 1998
Silty Mud 12 Mg 2.63         16 wt%ox The hemi-pelagic clay analyses where averaged over 10 m intervals and then averaged down-unit. Plank & Langmuir 1998
Silty Mud 25 Mn 0.59         16 wt%ox The hemi-pelagic clay analyses where averaged over 10 m intervals and then averaged down-unit. Plank & Langmuir 1998
Silty Mud 11 Na 2.42         16 wt%ox The hemi-pelagic clay analyses where averaged over 10 m intervals and then averaged down-unit. Plank & Langmuir 1998
Silty Mud 41 Nb 10         16 ppm The hemi-pelagic clay analyses where averaged over 10 m intervals and then averaged down-unit. Nb is calculated from Nb/Al for the Aleutian clastic turbidite. Plank & Langmuir 1998
Silty Mud 60 Nd 27.74         16 ppm The hemi-pelagic clay analyses where averaged over 10 m intervals and then averaged down-unit. Nd is calculated from the REE pattern in the Aleutian clastic turbidite. Plank & Langmuir 1998
Silty Mud 28 Ni 125.4         16 ppm The hemi-pelagic clay analyses where averaged over 10 m intervals and then averaged down-unit. Plank & Langmuir 1998
Silty Mud 15 P 0.2         16 wt%ox The hemi-pelagic clay analyses where averaged over 10 m intervals and then averaged down-unit. Plank & Langmuir 1998
Silty Mud 82 Pb 107.2         16 ppm The hemi-pelagic clay analyses where averaged over 10 m intervals and then averaged down-unit. Plank & Langmuir 1998
Silty Mud 37 Rb 56.8         16 ppm The hemi-pelagic clay analyses where averaged over 10 m intervals and then averaged down-unit. Rb is calculated from the continental ratio Rb/K2O = 40 because the Cr/Al2O3 and La/Al2O3 in the hemipelagic clay is typically continental. Plank & Langmuir 1998
Silty Mud 21 Sc 17         16 ppm The hemi-pelagic clay analyses where averaged over 10 m intervals and then averaged down-unit. Estimated value. Plank & Langmuir 1998
Silty Mud 14 Si 57.07         16 wt%ox The hemi-pelagic clay analyses where averaged over 10 m intervals and then averaged down-unit. SiO2 was calculated from the sum of major elements assuming a 10% LOI. Plank & Langmuir 1998
Silty Mud 62 Sm 6.07         16 ppm The hemi-pelagic clay analyses where averaged over 10 m intervals and then averaged down-unit. Sm is calculated from the continental ratio La/Sm =5.6 because the Cr/Al2O3 and La/Al2O3 in the hemipelagic clay is typically continental. Plank & Langmuir 1998
Silty Mud 38 Sr 184         16 ppm The hemi-pelagic clay analyses where averaged over 10 m intervals and then averaged down-unit. Plank & Langmuir 1998
Silty Mud 73 Ta 0.703         16 ppm The hemi-pelagic clay analyses where averaged over 10 m intervals and then averaged down-unit. Ta is calculated from the Nb/Ta = 15.2 ratio. Plank & Langmuir 1998
Silty Mud 90 Th 10.09         16 ppm The hemi-pelagic clay analyses where averaged over 10 m intervals and then averaged down-unit. Th is calculated from the continental ratio Th/Al2O3 = 0.66 because the Cr/Al2O3 and La/Al2O3 in the hemipelagic clay is typically continental. Plank & Langmuir 1998
Silty Mud 22 Ti 0.658         16 wt%ox The hemi-pelagic clay analyses where averaged over 10 m intervals and then averaged down-unit. Plank & Langmuir 1998
Silty Mud 92 U 4.44         16 ppm The hemi-pelagic clay analyses where averaged over 10 m intervals and then averaged down-unit. U is calculated from U/Th for the Aleutian clastic turbidite. Plank & Langmuir 1998
Silty Mud 23 V 212         16 ppm The hemi-pelagic clay analyses where averaged over 10 m intervals and then averaged down-unit. Plank & Langmuir 1998
Silty Mud 39 Y 28         16 ppm The hemi-pelagic clay analyses where averaged over 10 m intervals and then averaged down-unit. Y is calculated from 10*Yb. Plank & Langmuir 1998
Silty Mud 70 Yb 2.8         16 ppm The hemi-pelagic clay analyses where averaged over 10 m intervals and then averaged down-unit. Yb is calculated from the REE pattern in the Aleutian clastic turbidite. Plank & Langmuir 1998
Silty Mud 30 Zn 230.4         16 ppm The hemi-pelagic clay analyses where averaged over 10 m intervals and then averaged down-unit. Plank & Langmuir 1998
Silty Mud 40 Zr 145.4         16 ppm The hemi-pelagic clay analyses where averaged over 10 m intervals and then averaged down-unit. Zr is calculated from Zr/Al for the Aleutian clastic turbidite. Plank & Langmuir 1998
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