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Geology of the Gerlach--Hualapai Flat geothermal area, northwestern Nevada

Journal Article · · Q. Colo. Sch. Mines; (United States)
OSTI ID:6766243
The 500-square mile (1,280 square km) area around Gerlach and Hualapai Flat in northwestern Nevada includes Permo-Triassic metavolcanic and metasedimentary rocks disposed as roof pendants in Cretaceous granodiorite, Late Oligocene-Early Miocene rhyolitic, andesitic, and basaltic sequences, and Pliocene (.) and Quaternary alluvial and lacustrine sediments. The volcanic activity is far too old (23 my) to act as a source of heat in the area. Metasedimentary, granitic, volcanic, and alluvial clastic rocks may act as geothermal reservoirs. Thick lacustrine clays and alluvial-fluvial sediments as well as thick tuffaceous units have strong thermal insulating or cap rock properties. The location of the Gerlach hot springs is controlled by quasiradial spreading effected by contemporaneous activity on intersecting major regional normal faults. The location of Fly Ranch hot springs is also fault controlled and in addition is associated with modern tectonic rifting. Geothermal convection systems occur in the area, not by virtue of volcanic heating, but by trapping high regional heat flow beneath thermally insulating layers and by creating and maintaining open fractures by recurrent tensional tectonic activity.
OSTI ID:
6766243
Journal Information:
Q. Colo. Sch. Mines; (United States), Journal Name: Q. Colo. Sch. Mines; (United States) Vol. 73:3; ISSN QCSMA
Country of Publication:
United States
Language:
English