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Model for a deep conduit to the Beowawe geothermal system, Eureka and Lander Counties, Nevada

Conference · · Trans. - Geotherm. Resour. Counc.; (United States)
OSTI ID:6297874
;
A fault set trending N15-35W formed the eastern boundary of a major graben in the Beowawe area in the Late Tertiary. Geologic mapping and dipole-dipole resistivity data suggest that this fault set may have been and continues to be a deep conduit to the Beowawe geothermal system.
Research Organization:
Univ. of Utah Research Inst., Salt Lake City
OSTI ID:
6297874
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

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Related Subjects

15 GEOTHERMAL ENERGY
150201* -- Geology & Hydrology of Geothermal Systems-- USA-- (-1989)
ELECTRICAL SURVEYS
GEOLOGIC FAULTS
GEOLOGIC MODELS
GEOLOGIC STRUCTURES
GEOLOGY
GEOPHYSICAL SURVEYS
GEOTHERMAL SYSTEMS
HYDROTHERMAL ALTERATION
MAPPING
NEVADA
NORTH AMERICA
RESISTIVITY SURVEYS
SURVEYS
USA
WESTERN REGION