Delineation of an electrical resistivity anomaly, Malpais area, Beowawe KGRA, Eureka and Lander Counties, Nevada

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.

Data and Resources

Metadata Source

Additional Info

Field Value
Citation Date 1980-07-01T00:00:00

Harvest Information

Original ID ED1807897E024410B76C26452AFF26EC
Index Date 2016-03-17T20:52:41
Original Format ISO-USGIN
Original Version 1.2

Author

Name Smith, C.
Organization Utah Univ., Salt Lake City (USA). Earth Science Lab.
Email geoheat@oit.edu

Geographic Extent

North Bound 42.002207
South Bound 35.001857
East Bound -120.0064729
West Bound -114.0396479