Hydrogeochemistry of the northern Barbados accretionary complex transect: Ocean Drilling Project leg 110
- Univ. of California, San Diego, La Jolla, CA (United States)
- Univ. of Michigan, Ann Arbor (United States)
- 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), Vol. 95:B6, Issue B6; ISSN 0148-0227
- Country of Publication:
- United States
- Language:
- English
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GEOLOGIC FORMATIONS
GEOCHEMISTRY
INTERSTITIAL WATER
ISOTOPE RATIO
BASALT
BOREHOLES
CHLORIDES
GEOLOGIC FAULTS
HYDROGEN ISOTOPES
HYDROTHERMAL ALTERATION
OCEANIC CRUST
OXYGEN 18
OXYGEN ISOTOPES
SMECTITE
STRONTIUM 86
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VOLCANIC ROCKS
ALKALINE EARTH ISOTOPES
BETA DECAY RADIOISOTOPES
CAVITIES
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CHLORINE COMPOUNDS
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EVEN-EVEN NUCLEI
EVEN-ODD NUCLEI
GEOLOGIC FRACTURES
GEOLOGIC STRUCTURES
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HALOGEN COMPOUNDS
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HYDROGEN COMPOUNDS
IGNEOUS ROCKS
INTERMEDIATE MASS NUCLEI
ISLANDS
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LESSER ANTILLES
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STABLE ISOTOPES
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580000* - Geosciences