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

Ernst, W. G.; Paylor, Earnest D. II

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