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Application of a magnesium correction to the sodium-potassium-calcium geothermometer for selected thermal waters in southeastern Idaho

Conference · · Trans. - Geotherm. Resour. Counc.; (United States)
OSTI ID:6739764
Initial reservoir temperatures estimated by use of chemical geothermometers for thermal waters in southeastern Idaho generally result in poor agreement between the sodium-potassium-calcium and silica geothermometers. Concentrations of magnesium in these thermal waters ranged from 7.1 to 260 milligrams per liter. By applying a magnesium correction to the sodium-potassium-calcium geothermometer, estimated reservoir temperatures previously reported are reduced between 39/sup 0/ and 268/sup 0/C and result in much closer agreement between the sodium-potassium-calcium- and silica-estimated reservoir temperatures. Reservoir temperatures in southeastern Idaho probably do not exceed 128/sup 0/C.
Research Organization:
Geological Survey, Boise, Idaho
OSTI ID:
6739764
Report Number(s):
CONF-811015-
Conference Information:
Journal Name: Trans. - Geotherm. Resour. Counc.; (United States) Journal Volume: 5
Country of Publication:
United States
Language:
English