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Hydrothermal systems of the Wood River district, ID. [Abstract only]

Journal Article · · Geol. Soc. Am., Abstr. Programs; (United States)
OSTI ID:6020320

Hydrothermal systems of the Wood River district, central Idaho, have been studied by detailed geologic mapping and geochemical analyses of thermal and non-thermal waters. Integration of the results has led to thermal and non-thermal waters. Integration of the results has led to development of a target model for hydrothermal resources on the margin of the Idaho Batholith. Warfield Hot Springs, with temperatures up to 58/sup 0/C, flow from a major shear zone along the margin of an apophysis of the batholith. Hailey Hot Springs, with temperatures up to 60/sup 0/C, occur in an area of normal and thrust faults in the Paleozoic Milligen and Wood River Formations, 2.5 km from a highly brecciated batholith contact. Other Wood River district hydrothermal systems also occur along the margins of batholith apophyses or in adjacent highly fractured Paleozoic rocks. The Wood River district thermal waters are geochemically district from the local ground water. Thermal waters circulate through batholith rocks, with little or no equilibration with Paleozoic sedimentary or Tertiary volcanic rocks. The thermal waters are high F (11 to 19 ppM), low TDS (190 to 322 ppM) NaHCO/sub 3/-SO/sub 4/ waters, with up to half of the TDS as silica. The Magic Hot Springs system is higher TDS (about 1000 ppM) than the other sites. Geochemical thermometers for most systems are below 100/sup 0/C; Magic Hot Springs is about 150/sup 0/C. Thermal waters at the margin of the batholith are chemically similar to those in the interior of the batholith. The location of thermal systems at the margin of small apophyses of the Idaho Batholith is similar to other thermal systems in the western US. The waters circulate deep in the batholith rocks, and surface in either the intrusive or intruded rocks. Specific thermal systems are controlled by the most favorable fracture permeability for the circulation of water.

Research Organization:
Earth Science Lab., Salt Lake City, UT
OSTI ID:
6020320
Journal Information:
Geol. Soc. Am., Abstr. Programs; (United States), Journal Name: Geol. Soc. Am., Abstr. Programs; (United States) Vol. 15:5; ISSN GAAPB
Country of Publication:
United States
Language:
English