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• W4291719118 abstract "PreviousNext No AccessSecond International Meeting for Applied Geoscience & EnergyVariability in river-dominated deltaic systems: Facies models and drivers based on the Late Cretaceous Panther Tongue Sandstone, Central UtahAuthors: Clayton JacksDiane KamolaClayton JacksThe University of KansasSearch for more papers by this author and Diane KamolaThe University of KansasSearch for more papers by this authorhttps://doi.org/10.1190/image2022-3751820.1 SectionsAboutPDF/ePub ToolsAdd to favoritesDownload CitationsTrack CitationsPermissions ShareFacebookTwitterLinked InRedditEmail AbstractConceptual facies models are vital for making sedimentologic and stratigraphic interpretations in data poor settings. The Panther Tongue Sandstone (PT) of Central Utah has been cited as a type example for river-dominated deltaic depositional systems since the 1990’s. However, several significant questions and controversies relating to the PT’s depositional history and sequence stratigraphic framework persist. To address these questions and controversies, a field study of the PT’s full outcrop belt, focusing on understudied outcrops, was conducted. Data gathered include stratigraphic sections measured at the bed scale, interpreted photomosaics, paleocurrent indicators, and clinoform orientations. This data allows for the correlation of PT strata at the bedset scale within exposure localities, and at the lobe scale between exposure localities. It informs the following conclusions: The PT exhibits a significantly different outcrop expression in its northern extent (near Helper, UT/northern Book Cliffs), and southern extent (Huntington Canyon area/Wasatch Plateau). These strata are the deposits of a river-dominated delta with two end member depositional styles. In the north, sediment was emplaced by shelf turbidites as tabular, long-runout clinoforms; in the south, sediment was emplaced by avalanche flows as short- runout Gilbert-type delta front strata. The PT’s depositional system changed as it prograded southward primarily as the result of a relative fall in base level, which is marked in outcrop by a regionally extensive downlap surface.Keywords: River dominated delta, facies, sequence stratigraphy, Cretaceous, UtahPermalink: https://doi.org/10.1190/image2022-3751820.1FiguresReferencesRelatedDetails Second International Meeting for Applied Geoscience & EnergyISSN (print):1052-3812 ISSN (online):1949-4645Copyright: 2022 Pages: 3694 publication data© 2022 Published in electronic format with permission by the Society of Exploration Geophysicists and the American Association of Petroleum GeologistsPublisher:Society of Exploration Geophysicists HistoryPublished Online: 15 Aug 2022 CITATION INFORMATION Clayton Jacks and Diane Kamola, (2022), Variability in river-dominated deltaic systems: Facies models and drivers based on the Late Cretaceous Panther Tongue Sandstone, Central Utah, SEG Technical Program Expanded Abstracts : 2483-2486. https://doi.org/10.1190/image2022-3751820.1 Plain-Language Summary KeywordsRiver dominated deltafaciessequence stratigraphyCretaceousUtahPDF DownloadLoading ..." @default.
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• W4291719118 title "Variability in river-dominated deltaic systems: Facies models and drivers based on the Late Cretaceous Panther Tongue Sandstone, Central Utah" @default.
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