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- W126011014 abstract "Petrologic and stable isotope geochemical studies were conducted on well cuttings from a Sulphur Banks tract steam well in the Geysers. The observed hydrothermal mineral zonation is indicative of an extremely hot (>300/sup 0/C) water-dominated geothermal system characterized by high fluid flow associated with fault contacts. Strata within the steam reservoir are not distinguished by diagnostic steam-derived secondary alteration products. However, a late stage generation of calcite was interpreted to have been deposited during the transition of the reservoir fluid to the vapor phase. The distribution of this material is restricted to a shallow zone (<600m) corresponding to the shallow steam anomaly reported in the Sulphur Banks area." @default.
- W126011014 created "2016-06-24" @default.
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- W126011014 date "1982-10-01" @default.
- W126011014 modified "2023-09-23" @default.
- W126011014 title "Mineral zonation and stable isotope geochemistry of a production well in the Geysers Geothermal field, California" @default.
- W126011014 hasPublicationYear "1982" @default.
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