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dc.contributor.advisorShelton, John N.
dc.contributor.authorMorganelli, Daniel
dc.date.accessioned2015-10-14T21:37:36Z
dc.date.available2015-10-14T21:37:36Z
dc.date.issued1976-05-01
dc.identifier.urihttps://hdl.handle.net/11244/19619
dc.description.abstractThe primary purpose of this study is to describe the geometry and internal features of the uppermost part of the Vamoosa Formation in north-central Oklahoma and interpret its trend and genesis. A secondary objective is to determine gross depositional trends in the overlying Lecompton Limestone. Included in the thesis are correlation sections, measured sections, thickness maps, paleocurrent diagrams, and petrographic features.
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.titleDepositional Environment and Trend of the Uppermost Part of the Vamoosa Formation and Lecompton Limestone in the Eastern Part of North-Central Oklahoma
dc.typetext
dc.contributor.committeeMemberTrammell, John
dc.contributor.committeeMemberStewart, Gary F.
osu.filenameThesis-1976-M849d.pdf
osu.accesstypeOpen Access
dc.description.departmentGeology
dc.type.genreThesis


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