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dc.contributor.authorWright, Sarah N
dc.date.accessioned2018-06-14T04:30:14Z
dc.date.available2018-06-14T04:30:14Z
dc.date.issued2017-12
dc.identifier.otherwright_sarah_n_201712_ms
dc.identifier.urihttp://purl.galileo.usg.edu/uga_etd/wright_sarah_n_201712_ms
dc.identifier.urihttp://hdl.handle.net/10724/38248
dc.description.abstractThe Jurassic Windy Hill Sandstone in Wyoming contains features consistent with deposition on an open-coast tidal flat, like those along the coast of Korea today, and this study uses field and UAV-based methods to investigate the sequence stratigraphic context of these deposits. Surfaces of forced regression are present and indicate deposition in the FSST and LST, re-enforcing the idea that tidal deposition can occur in many contexts. The recognition of surfaces of forced regression at stratigraphic positions previously interpreted as the J5 unconformity suggest that this surface may be at a stratigraphically higher position, implying that portions of the Redwater Shale, Windy Hill Sandstone, and Morrison Formation are contemporaneous in Wyoming. The Morrison Formation displays continuous progradation that is attributed to a slowed rate of tectonic subsidence, illustrating how tectonics can result in deviations from predicted sequence stratigraphic architecture, with the TST apparently absent from the rock record
dc.languageeng
dc.publisheruga
dc.rightsOn Campus Only Until 2019-12-01
dc.subjectSequence Stratigraphy
dc.subjectFalling Stage Systems Tract
dc.subjectTidal Flat
dc.subjectUAV
dc.subjectWindy Hill Sandstone
dc.subjectSundance Formation
dc.titleThe falling-stage progradation of an open-coast tidal flat:
dc.title.alternativeUAV-assisted sequence stratigraphy of the Jurassic windy hill sandstone, Wyoming U.S.A.
dc.typeThesis
dc.description.degreeMS
dc.description.departmentGeology
dc.description.majorGeology
dc.description.advisorSteven Holland
dc.description.committeeSteven Holland
dc.description.committeeDavid S. Leigh
dc.description.committeeClark Alexander


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