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- W2069179878 abstract "Fluid inclusions (191) in calcite, quartz, K-feldspar, and epidote from ≈l-mm veinlets in cores and well cuttings from 604–2560 m homogenize from 217° to >500°C and vary widely in salinity, suggesting a complex history of fluids surrounding these samples. No daughter minerals were seen, and no clathrates were recognized on freezing. Vapor-rich inclusions under pressure, presumably containing CO2 and/or CH4, were found from a wide range of depths, suggesting that effervescence has occurred. Low-salinity fluids (1.2 –4.0 wt % NaCl eq) were present as deep as 1939 m. The data can be explained by a combination of processes such as thermal metamorphism of evaporites and other sediments and mixing of water from metamorphic dehydration reactions with partly evaporated Colorado River water." @default.
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- W2069179878 date "1988-11-10" @default.
- W2069179878 modified "2023-10-05" @default.
- W2069179878 title "Fluid Inclusions in Salton Sea Scientific Drilling Project Core: Preliminary Results" @default.
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- W2069179878 doi "https://doi.org/10.1029/jb093ib11p13159" @default.
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