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U.S. Department of Energy
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Subsurface geology of the Raft River geothermal area, Idaho

Conference · · Trans. - Geotherm. Resour. Counc.; (United States)
OSTI ID:6167814
The Raft River Valley occupies an upper Cenozoic structural basin filled with nearly 1600 m of fluvial silt, sand, and gravel. Rapid facies and thickness changes, steep initial dips (30/sup 0/C), and alteration make correlation of basin-fill depositional units very difficult. Hydrothermal alteration products in the form of clays and zeolites, and deposition of secondary calcite and silica increase with depth. The abundance of near-vertical open fractures also increases with depth, allowing greater movement of hydrothermal fluids near the base of the Cenozoic basin fill. The basin is floored with quartzites and schists that can be correlated with formations in the nearby Raft River Range. Beneath these rocks is a Precambrian adamellite basement complex. The Raft River geothermal system is a hot water convective system relying on deep circulation of meteoric water in a region of high geothermal gradients and open fractures near the base of the Tertiary basin fill.
Research Organization:
Geological Survey, Denver, CO
OSTI ID:
6167814
Report Number(s):
CONF-800920-
Conference Information:
Journal Name: Trans. - Geotherm. Resour. Counc.; (United States) Journal Volume: 4
Country of Publication:
United States
Language:
English