FN Archimer Export Format
PT J
TI Geochemical Significance of Diagenetic Reactions in Ocean Sediments: An Evaluation of Interstitial Water Data (Extended Abstract)
BT 
AF GIESKES, J M
   LAWRENCE, J R
AS 1:;2:;
FF 1:;2:;
IF 0.662
TC 0
UR https://archimer.ifremer.fr/doc/00246/35695/34203.pdf
LA English
DT Article
AB 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.
PY 1981
SO Oceanologica Acta, Special issue
SN 0399-1784
PU Gauthier-Villars
ID 35695
ER

EF