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- W2016458399 abstract "Abstract The oxygen isotopic fractionation between sulfate ion and water is a useful measure of the temperature of geothermal reservoirs. The rate of the oxygen isotopic exchange reaction between sulfate and water in acid to neutral thermal waters of a temperature of 100°C or higher is sufficiently fast to justify that the sulfates are in isotopic equilibrium with the reservoir waters. The isotopic thermometer has been successfully applied to several Japanese geothermal fields. The temperatures measured by this method are in good agreement with silica and alkali-temperatures. Some factors affecting the results as well as the analytical techniques of the oxygen isotopic analyses of sulfates are discussed." @default.
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- W2016458399 date "1977-01-01" @default.
- W2016458399 modified "2023-09-26" @default.
- W2016458399 title "Sulfate-water isotope thermometry applied to geothermal systems" @default.
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- W2016458399 doi "https://doi.org/10.1016/0375-6505(77)90010-4" @default.
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