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Ground-Level Magnetic Study of Greene County, Ohio

Please use this identifier to cite or link to this item: http://hdl.handle.net/1811/22762

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dc.creator Obot, V. E. D. en_US
dc.creator Wolfe, Paul J. en_US
dc.date.accessioned 2006-07-07T01:55:27Z
dc.date.available 2006-07-07T01:55:27Z
dc.date.issued 1981-03 en_US
dc.identifier.citation The Ohio Journal of Science. v81, n2 (March, 1981), 50-54 en_US
dc.identifier.issn 0030-0950 en_US
dc.identifier.uri http://hdl.handle.net/1811/22762
dc.description Author Institution: Department of Physics, Wright State University en_US
dc.description.abstract We performed a ground level geomagnetic survey of Greene County, Ohio in the fall of 1976. The geomagnetic map showed a positive magnetic anomaly running from the northwestern section to the southeastern section of the county while the remainder of the map was relatively undisturbed. We analyzed the localized anomaly of the southeastern section by the Peters methods and by fitting to the model of a vertical rectangular prism magnetized along the earth's field. The Peters slope and half-slope methods gave maximum depth limits to the top of the body of 1.16 km and 1.08 km respectively. The best fit to the vertical prism model yielded a depth of 1.04±0.05 km, a width of 2.5 ±0.2 km, and a susceptibility contrast of +0.0039 cgs units. From the depth, we concluded that the source of the anomalies is intrabasement susceptibility variations. en_US
dc.format.extent 364929 bytes
dc.format.mimetype application/pdf
dc.language.iso en_US
dc.title Ground-Level Magnetic Study of Greene County, Ohio en_US