Show simple item record

dc.creatorObot, V. E. D.en_US
dc.creatorWolfe, Paul J.en_US
dc.date.accessioned2006-07-07T01:55:27Z
dc.date.available2006-07-07T01:55:27Z
dc.date.issued1981-03en_US
dc.identifier.citationThe Ohio Journal of Science. v81, n2 (March, 1981), 50-54en_US
dc.identifier.issn0030-0950en_US
dc.identifier.urihttp://hdl.handle.net/1811/22762
dc.descriptionAuthor Institution: Department of Physics, Wright State Universityen_US
dc.description.abstractWe 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.extent364929 bytes
dc.format.mimetypeapplication/pdf
dc.language.isoen_US
dc.titleGround-Level Magnetic Study of Greene County, Ohioen_US


Files in this item

Thumbnail

Items in Knowledge Bank are protected by copyright, with all rights reserved, unless otherwise indicated.

This item appears in the following Collection(s)

Show simple item record