Oxygen, carbon and strontium isotope data for DSDP Hole 35-323

A downhole decrease in 18O, Mg(2+) and K+, an increase in Ca(2+) and a low 87Sr/86Sr ratio of 0.7067 in the pore fluids of DSDP site 323 were caused principally by the alteration of volcanic material. These chemical and isotopic patterns were produced by the alteration, in order of decreasing import...

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Bibliographic Details
Main Authors: Lawrence, James R, Drever, James I, Anderson, Thomas F, Brueckner, H K
Format: Dataset
Language:English
Published: PANGAEA 1979
Subjects:
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.706890
https://doi.org/10.1594/PANGAEA.706890