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Study of the Reed Dolomite Aided by Remotely Sensed Imagery, Central White-Inyo Range, Easternmost California

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dc.contributor.author Ernst, W. G. en_US
dc.contributor.author Paylor, Earnest D. II en_US
dc.date.accessioned 2004-09-30T04:25:54Z
dc.date.available 2004-09-30T04:25:54Z
dc.date.issued 1996 en_US
dc.identifier.clearanceno 96-0549 en_US
dc.identifier.uri http://hdl.handle.net/2014/24733
dc.description.abstract Remote-sensing methods are of great value in assessing the stratigraphy and geologic structure of inaccessible terrains, especially where lithologic contrasts are marked. In this report, we show that such techniques can be successfully applied to a massive carbonate unit, the Reed Dolomite, exposed in the Wacuoba Mountain, Blanco Mountain, and Mount Barcroft quadrangles of east-central California. en_US
dc.format.extent 889836 bytes
dc.format.mimetype application/pdf
dc.language.iso en_US
dc.subject.other Remote-sensing stratigraphy geology lithologic contrasts the Reed Dolomite en_US
dc.title Study of the Reed Dolomite Aided by Remotely Sensed Imagery, Central White-Inyo Range, Easternmost California en_US


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