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dc.contributor.advisorShelton, John W.
dc.contributor.authorCheung, Paul Kwong-Shun
dc.date.accessioned2015-09-23T18:29:26Z
dc.date.available2015-09-23T18:29:26Z
dc.date.issued1978-05-01
dc.identifier.urihttps://hdl.handle.net/11244/18545
dc.description.abstractThis thesis is a study of the geothermal gradient in the sedimentary-rock column in Oklahoma, exclusive of the Panhandle and the southeasternmost and the northeasternmost parts. Data used are temperature measurements in boreholes drilled for oil and gas. Maps prepared portray the temperature gradients in the normally pressured formations for the State of Oklahoma and the temperature gradients in the abnormally pressured strata in the Anadarko and Ardmore basins. These maps are thought to provide useful information of the subsurface temperature conditions in Oklahoma.
dc.formatapplication/pdf
dc.languageen_US
dc.publisherOklahoma State University
dc.rightsCopyright is held by the author who has granted the Oklahoma State University Library the non-exclusive right to share this material in its institutional repository. Contact Digital Library Services at lib-dls@okstate.edu or 405-744-9161 for the permission policy on the use, reproduction or distribution of this material.
dc.titleGeothermal Gradient in Sedimentary Rocks in Oklahoma
dc.typetext
dc.contributor.committeeMemberStewart, Gary F.
dc.contributor.committeeMemberKent, Douglas C.
osu.filenameThesis-1978-C526g.pdf
osu.accesstypeOpen Access
dc.description.departmentGeology
dc.type.genreThesis


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