Delineation of an electrical resistivity anomaly, Malpais area, Beowawe KGRA, Eureka and Lander Counties, Nevada [electronic resource]
Geothermal Legacy.
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Online Access |
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| Format: | Government Document Electronic eBook |
| Language: | English |
| Published: |
Salt Lake City, Utah : Oak Ridge, Tenn. :
University of Utah. Research Institute. Earth Science Laboratory ; distributed by the Office of Scientific and Technical Information, U.S. Dept. of Energy,
1980.
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| Subjects: |
MARC
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| 245 | 0 | 0 | |a Delineation of an electrical resistivity anomaly, Malpais area, Beowawe KGRA, Eureka and Lander Counties, Nevada |h [electronic resource] |
| 260 | |a Salt Lake City, Utah : |b University of Utah. Research Institute. Earth Science Laboratory ; |a Oak Ridge, Tenn. : |b distributed by the Office of Scientific and Technical Information, U.S. Dept. of Energy, |c 1980. | ||
| 300 | |a Pages: 30 : |b digital, PDF file. | ||
| 336 | |a text |b txt |2 rdacontent. | ||
| 337 | |a computer |b c |2 rdamedia. | ||
| 338 | |a online resource |b cr |2 rdacarrier. | ||
| 500 | |a Published through the Information Bridge: DOE Scientific and Technical Information. | ||
| 500 | |a 07/01/1980. | ||
| 500 | |a "doe/id/12079-7" | ||
| 500 | |a Smith, C. | ||
| 520 | 3 | |a A simple numerical model of previously released bipole-dipole resistivity data shows the margin of the graben to be anomalously conductive below the Malpais. The conductive area has been delineated with data from a dipole-dipole resistivity survey run in April 1980 for this study. Detailed numerical models of these data define a 1250 m wide body with resistivities less than 20 ohm-m that appear to connect The Geysers and the graben boundary. The minimum depth to the conductor is interpreted to be 375 m; its depth extent is undetermined. The electrical data do not resolve whether the anomaly below the Malpais may be the product of a defunct hydrothermal system or the signature of an active system. If thermal gradient data detect an enhanced heat flow anomaly in the same area, the Malpais may be a viable geothermal exploration target within the Beowawe KGRA. | |
| 520 | 0 | |a Geothermal Legacy. | |
| 536 | |b AC07-80ID12079. | ||
| 650 | 7 | |a Water Springs. |2 local. | |
| 650 | 7 | |a Nevada. |2 local. | |
| 650 | 7 | |a Geothermal Systems. |2 local. | |
| 650 | 7 | |a Western Region. |2 local. | |
| 650 | 7 | |a Hydrothermal Systems. |2 local. | |
| 650 | 7 | |a Mathematical Models. |2 local. | |
| 650 | 7 | |a Geology. |2 local. | |
| 650 | 7 | |a Kgra. |2 local. | |
| 650 | 7 | |a Electrical Surveys. |2 local. | |
| 650 | 7 | |a Geophysical Surveys. |2 local. | |
| 650 | 7 | |a Surveys. |2 local. | |
| 650 | 7 | |a Usa. |2 local. | |
| 650 | 7 | |a Resistivity Surveys. |2 local. | |
| 650 | 7 | |a North America. |2 local. | |
| 650 | 7 | |a Maps. |2 local. | |
| 650 | 7 | |a Thermal Springs. |2 local. | |
| 650 | 7 | |a Geysers. |2 local. | |
| 650 | 7 | |a Hot Springs. |2 local. | |
| 650 | 7 | |a Geothermal Energy. |2 edbsc. | |
| 710 | 2 | |a University of Utah. |b Research Institute. |b Earth Science Laboratory. |4 res. | |
| 710 | 1 | |a United States. |b Department of Energy. |b Office of Scientific and Technical Information. |4 dst. | |
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