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Hydrogeochemistry of the northern Barbados accretionary complex transect: Ocean Drilling Project leg 110

Journal Article · · Journal of Geophysical Research; (United States)
 [1];  [2];  [3]
  1. Univ. of California, San Diego, La Jolla, CA (United States)
  2. Univ. of Michigan, Ann Arbor (United States)
  3. Univ. Louis Pasteur, Strasbourg (France)
Detailed studies of the major element geochemistry, oxygen and hydrogen isotope ratios of pore fluids, and the {sup 87}Sr/{sup 86}Sr ratio of dissolved strontium have made it possible to unravel physical and chemical processes that affect the pore fluid chemistry in a transect of drill holes across the northern Barbados accretionary complex. These processes include (1) alteration of volcanic ash buried in the Pleisticene-Pliocene sediment column; (2) alteration of underlying basalts of layer 2 of the oceanic crust; (3) movement of fluids from deep in the accretionary complex along fault zones (particularly the decollement) and minor permeable layers; these fluids from deeper in the complex are characterized by low chloride concentrations and increased {sup {delta}18}O(H{sub 2}O) values, presumably as a result of dehydration of smectite interlayers; and (4) mixing processes involving the migrating fluids cause incongruities in the geochemical anomalies of these fluids.
OSTI ID:
5073575
Journal Information:
Journal of Geophysical Research; (United States), Journal Name: Journal of Geophysical Research; (United States) Journal Issue: B6 Vol. 95:B6; ISSN 0148-0227; ISSN JGREA
Country of Publication:
United States
Language:
English