Article thumbnail

Geochemical Significance of Diagenetic Reactions in Ocean Sediments: An Evaluation of Interstitial Water Data (Extended Abstract)

By J M Gieskes and J R Lawrence

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

Publisher: Gauthier-Villars
Year: 1981
OAI identifier: oai:archimer.ifremer.fr:35695
Download PDF:
Sorry, we are unable to provide the full text but you may find it at the following location(s):
  • https://archimer.ifremer.fr/do... (external link)
  • https://archimer.ifremer.fr/do... (external link)
  • Suggested articles


    To submit an update or takedown request for this paper, please submit an Update/Correction/Removal Request.