| Type |
Article |
| Date |
1981 |
| Language |
English |
| Author(s) |
Gieskes J M, Lawrence J R |
| Meeting |
26. Int. Geological Congress, Paris (France), 7 Jul 1980 |
| Source |
Oceanologica Acta, Special issue (0399-1784) (Gauthier-Villars), 1981 |
| Abstract |
The gradients of dissolved calcium and magnesium, as well as those of delta super(18)O of the interstitial waters in deep sea sediments imply fluxes of material from layer 2 (oceanic basalts) into layer 1 (sediments) and vice versa. Especially the flux of H sub(2) super(18)O into layer 2 is significant and allows an estimate of the degree of alteration of layer 2 of the oceanic crust. |
| Full Text |
| File |
Pages |
Size |
Access |
| 34203.pdf |
4 |
567 KB |
Open access |
|
