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• W2102752950 abstract "Abstract Detailed facies-architecture study of a portion of a > 10-kilometer-wide compound incised valley in outcrops of the Turonian Ferron Notom Delta shows three simple incised valleys filled with different facies associations. The valley-fill deposits were mapped with 30 detailed measured sections, photomosaics, and bedding diagrams. The oldest, incised valley 3, forms a terrace deposit that erodes directly into hummocky-cross-bedded lower-shoreface deposits. It is filled with fine- to medium-grained tidally influenced deposits, characterized by abundant mud-draped cross beds, sparse burrowing, and a bimodal paleocurrent-direction pattern. The younger incised valley 2 locally cuts through the valley 3 terrace and also into the lower-shoreface deposits. The valley 2 fill comprises multi-story medium-grained fluvial deposits with minor finer-grained tidally influenced fluvial deposits in the upper 10%. The youngest, incised valley 1, also locally cuts into the lower-shoreface deposits, removing the terraces formed by valleys 2 and 3. Valley 1 is filled entirely with medium-grained fluvial deposits. The composite valley fill records generally increasing fluvial dominance and decreasing tidal influence during successive cut-and-fill episodes associated with each simple valley fill. It is hypothesized to correlate with a longer-term, stepped relative fall of sea level, punctuated by standstills, or minor rises of sea level." @default.
• W2102752950 created "2016-06-24" @default.
• W2102752950 creator A5023578647 @default.
• W2102752950 creator A5089206039 @default.
• W2102752950 date "2013-04-09" @default.
• W2102752950 modified "2023-09-23" @default.
• W2102752950 title "Facies-Architecture Study of A Stepped, Forced Regressvie Compound Incised Valley In the Ferron Notom Delta, Southern Central Utah, U.S.A" @default.
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• W2102752950 doi "https://doi.org/10.2110/jsr.2013.19" @default.
• W2102752950 hasPublicationYear "2013" @default.
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