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dc.creatorParr, David F.en_US
dc.creatorChang, Luke L. Y.en_US
dc.date.accessioned2006-07-07T01:50:11Z
dc.date.available2006-07-07T01:50:11Z
dc.date.issued1980-01en_US
dc.identifier.citationThe Ohio Journal of Science. v80, n1 (January, 1980), 20-29en_US
dc.identifier.issn0030-0950en_US
dc.identifier.urihttp://hdl.handle.net/1811/22668
dc.descriptionAuthor Institution: Department of Geology, Miami Universityen_US
dc.description.abstractTwo sulfate minerals, barite and celestite, were identified in the Devonian rocks at Pugh Quarry. The barite occurs commonly as rosette-like clusters with wide variety of colors and crystal habits. Unusual features include paired crystals and hollow crystals. The former consist of two barite crystals growing parallel with each other on the dolostone matrix, and the latter only of a thin wall of barite commonly marked by cross striations. Celestite crystals have two different colors. The grayblue and blue crystals are prismatic to blocky and occur as well-formed individuals, whereas the colorless and white crystals are tabular to bladed and occur as distinct individuals and as compact clusters.en_US
dc.format.extent4466976 bytes
dc.format.mimetypeapplication/pdf
dc.language.isoen_US
dc.titleDescriptive Mineralogy of Pugh Quarry, Northwestern Ohio: Barite and Celestiteen_US


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