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Soda Lake, Nevada, Thermal Anomaly

Hill, D. G.; Layman, E. B.; Swift, C. M.; Yungul, S. H.

Key words
Exploration; Reservoir; Resource Potential; USA; Nevada; Soda Lake; Thermal Anomaly; Fault Control; 400 F; Geothermometers; Geology; Stratigraphy; Seismic Data; Magneto Telluric; Plume; Hydrology
Location
Soda Lake, Nevada
Conference
Geothermal Resources Council Transactions
Year
1979
Session
Exploration; Stratigraphy; Geophysical surveys; Geological s
Language
English

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Abstract

The Soda Lake thermal anomaly is located in the southern part of the extensional Carson Sink in Western Nevada. The shallow thermal regime is well defined, with temperatures in excess of 365°F in exploratory temperature holes. Current interpretation of all available data yields a NE-SW trending thermal plume dipping to the SE. This plume appears to rise along the NE-SW trending fault, NE of Soda Lake. Geochemical base temperature determinations estimate Reservoir temperature in excess of 400°F. Additionally work is underway to define and evaluate the potential geothermal reservoir.

Copyright 1979, Geothermal Resources Council. Readers who download papers from this site should honour the copyright of the original authors, and may not copy or distribute the work further without the permission of the original publisher.

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