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- W279080908 abstract "More than 65 boreholes, 1.5 to 3.5 km deep have encountered temperatures less than or equal to 350/sup 0/C and brines with less than or equal to 1% total dissolved solids in the Cerro Prieto geothermal field of the Salton Trough intracontinental rift system. Temperature-dependence dehydration and decarbonation reactions have produced progressive hydrothermal alteration in the deltaic sediments of the reservoir to form greenschist facies rocks. Various methods of geothermometry were applied, including authigenic mineral assemblages and light stable isotopes, to study temperature distribution and fluid-rock interaction in the subsurface. These data have revealed a pattern of mineral zones and isotopic ratios in the rocks which defines the shape of the reservoir and records the pattern of hydrothermal circulation prior to production. It was inferred that a thermal plume, elongated in a NW-SE direction, dips at 45/sup 0/ to the NE; it is recharged from the NE and discharges to the SW." @default.
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- W279080908 date "1980-09-01" @default.
- W279080908 modified "2023-09-26" @default.
- W279080908 title "Hydrothermal alteration as an indicator of temperature and flow regime in the Cerro Prieto geothermal field of Baja California" @default.
- W279080908 hasPublicationYear "1980" @default.
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