1986
DOI: 10.3133/ofr86432
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Geophysical surveys in the vicinity of the Pinson and Getchell mines, Humboldt County, Nevada

Abstract: This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and stratigraphic nomenclature. Any use of trade names is for descriptive purposes only and does not imply endorsement by the U.S. Geological Survey.

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Cited by 2 publications
(3 citation statements)
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“…Ground-based electrical, magnetic, and gravity data collected before the airborne surveys were flown are presented in Abrams and others (1984), Reran and Smith (1984), Reran andMcCafferty (1986), and others (1984;. The gravity data reported in Abrams and others (1984) are partly superseded by the profile data presented here (discussed below).…”
mentioning
confidence: 77%
See 1 more Smart Citation
“…Ground-based electrical, magnetic, and gravity data collected before the airborne surveys were flown are presented in Abrams and others (1984), Reran and Smith (1984), Reran andMcCafferty (1986), and others (1984;. The gravity data reported in Abrams and others (1984) are partly superseded by the profile data presented here (discussed below).…”
mentioning
confidence: 77%
“…coverage of the airborne data would have been prohibitively expensive. The profiles collected for Battle Mountain Gold were part of the company's exploration program.Ground-based electrical, magnetic, and gravity data collected before the airborne surveys were flown are presented in Abrams and others (1984), Reran and Smith (1984), Reran andMcCafferty (1986), and others (1984;. The gravity data reported in Abrams and others (1984) are partly superseded by the profile data presented here (discussed below).The Getchell digital airborne geophysical data were originally released through the U.S. Department of Commerce's National Geophysical Data Center in February, 1989.…”
mentioning
confidence: 99%
“…Ground magnetic and various electromagnetic methods may be used to map faults, fractures, and highly permeable altered zones that may serve as ground water conduits (Heran and Smith, 1984;Heran and McCafferty, 1986;Hoover and others, 1986;Hoekstra and others, 1989). Electrical resistivity methods can delineate hydrothermally altered areas and fault zones as resistivity lows and silicified rock as resistivity highs (Hallof, 1989;Hoekstra and others, 1989;Corbett, 1990).…”
Section: Geoenvironmental Geophysicsmentioning
confidence: 99%