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Precambrian Quartzo-Feldspathic Gneiss from the Herman 1A Well, Erie County, Ohio

Please use this identifier to cite or link to this item: http://hdl.handle.net/1811/5682

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dc.creator Ross, Martin E. en_US
dc.date.accessioned 2005-10-01T03:20:24Z
dc.date.available 2005-10-01T03:20:24Z
dc.date.issued 1972-03 en_US
dc.identifier.citation The Ohio Journal of Science. v72 n2 (March, 1972), 105-109 en_US
dc.identifier.issn 0030-0950 en_US
dc.identifier.uri http://hdl.handle.net/1811/5682
dc.description Author Institution: Department of Geology, Kent State University, Kent, Ohio 44240 en_US
dc.description.abstract Precambrian quartzo-feldspathic gneiss was encountered at an elevation of —3616 feet in the Herman 1A well drilled in southeastern Erie County, Ohio, by the Amerada Petroleum Corporation. The five samples of this gneiss that were studied exhibit varying degrees of gneissose foliation. In order of decreasing abundance, microcline, plagioclase, quartz, and biotite together account for an average of 75% of the mineralogy. Greenish saussuritized plagioclase in layers and veins is abundant in three of the samples. Based on the presence of minor amounts of garnet, a plagioclase composition of An36, and the location of the well, the gneiss is considered to lie within the Grenville orogenic belt of high-grade, regionally metamorphosed rock. en_US
dc.format.extent 1170663 bytes
dc.format.mimetype application/pdf
dc.language.iso en_US
dc.rights Reproduction of articles for non-commercial educational or research use granted without request if credit to The Ohio State University and The Ohio Academy of Science is given. en_US
dc.title Precambrian Quartzo-Feldspathic Gneiss from the Herman 1A Well, Erie County, Ohio en_US