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Geothermometry and water-rock interaction in selected thermal systems in the Cascade Range and Modoc Plateau, western United States

Journal Article · · Geothermics (International Journal of Geothermal Research and its Applications); (United States)
; ;  [1]
  1. Geological Survey, Menlo Park, CA (United States)
The sulfate-water isotope geothermometer indicates higher equilibrium temperature than the silica or cation ratio geothermometer for the Na-Cl and Na-Ca-Cl thermal waters of the Cascade Range, Oregon and the Na-SO[sub 4] thermal waters of the Modoc Plateau, northeastern California. Sulfate concentrations in the Na-Ca-Cl waters decrease as [delta][sup 18]O values of the dissolved sulfate become more depleted; conversely, sulfate concentrations in the Na-SO[sub 4] waters increase as [delta][sup 18]O values of the sulfate become more depleted. Calculations show that the thermal waters are theoretically saturated with respect to anhydrite (CaSO[sub 4]) at temperature very close to those calculated from the sulfate-water isotope geothermometer.
OSTI ID:
6093836
Journal Information:
Geothermics (International Journal of Geothermal Research and its Applications); (United States), Journal Name: Geothermics (International Journal of Geothermal Research and its Applications); (United States) Vol. 22:1; ISSN GTMCAT; ISSN 0375-6505
Country of Publication:
United States
Language:
English