from R.S.Taylor, 1966
Element | Cu | Ni | Co | Cr | V | Y | U | Zr | Mo | W | Zn | Au(ppb) | Ag | Hg |
Basalt | 100 | 150 | 50 | 200 | 250 | 25 | 0.6 | 150 | 1 | 1 | 100 | 4 | 0.1 | 0.1 |
Ultramafic | 10 | 2000 | 150 | 2000 | 50 | – | >1 | 50 | >1 | >1 | 50 | 5 | 0.1 | – |
Granodirorite | 30 | 20 | 10 | 20 | 100 | 30 | 3 | 140 | 1 | 2 | 60 | 4 | 0.1 | 0.1 |
Granite | 10 | >1 | 1 | 4 | 20 | 40 | 5 | 180 | 2 | 2 | 40 | 4 | 0 | 0.1 |
Shale | 50 | 70 | 20 | 100 | 130 | 25 | 4 | 160 | 3 | 2 | 100 | 4 | 0.5 | 0.5 |
Greywacke | 40 | 50 | 20 | 140 | 70 | 30 | 3 | 140 | – | 2 | 50 | 4 | 0.5 | 0.1 |
Limestone | 15 | 12 | 10 | 10 | 15 | 15 | 2 | 20 | 1 | 0.5 | 25 | 5 | 1 | 0.1 |