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- W2050247059 abstract "Analysis of sulfur and oxygen isotopic compositions of dissolved sulfate from a vertical water profile in the anoxic, hypersaline Orca Basin provides important constraints upon the provenance of the sulfate. Results support a dissolution origin of the brine from a Jurassic evaporitic salt. However, mass balance considerations and the observed minima in the vertical δ18O-sulfate profile at the brine-seawater interface are not reconcilable with only a simple two box brine-seawater mixing model. Instead, the data imply contributions from the oxidation of sulfides." @default.
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- W2050247059 date "1988-01-01" @default.
- W2050247059 modified "2023-09-24" @default.
- W2050247059 title "Sulfur and oxygen isotopic compositions of dissolved sulfate in the Orca Basin: Implications for origin of the high-salinity brine and oxidation of sulfides at the brine-seawater interface" @default.
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- W2050247059 doi "https://doi.org/10.1016/0025-3227(88)90115-6" @default.
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