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The American Upper Ordovician Standard. XVI, Utility of Clastic-Ratio Values to Distinguish Kope and Fairview Formations, Hamilton County, Ohio

Please use this identifier to cite or link to this item: http://hdl.handle.net/1811/5648

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dc.creator Osborne, Robert H. en_US
dc.date.accessioned 2005-10-01T03:10:27Z
dc.date.available 2005-10-01T03:10:27Z
dc.date.issued 1971-09 en_US
dc.identifier.citation The Ohio Journal of Science. v71 n5 (September, 1971), 317-319 en_US
dc.identifier.issn 0030-0950 en_US
dc.identifier.uri http://hdl.handle.net/1811/5648
dc.description Author Institution: Department of Geological Sciences, University of Southern California, Los Angeles, California 90007 en_US
dc.description.abstract The result of a Mann-Whitney U-test indicates that clastic-ratio values for the Kope Formation are stochastically greater than are those for the Fairview Formation in eastern Hamilton County, Ohio. The use of the clastic-ratio as an inferential statistic when applied to these formations is justified. en_US
dc.format.extent 211922 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 The American Upper Ordovician Standard. XVI, Utility of Clastic-Ratio Values to Distinguish Kope and Fairview Formations, Hamilton County, Ohio en_US