Titlebook: Seismic Facies and Sedimentary Processes of Submarine Fans and Turbidite Systems; Paul Weimer,Martin H. Link Book 1991 Springer Science+Bu

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Paleontologic Constraints on Depositional Modeling: Examples of Integration of Biostratigraphy and S within successive depositional cycles. Each step in the interpretational process requires critical evaluation and cross-correlation of the data. Two examples of this procedure are presented, both from the Pliocene-Pleistocene Galveston-High Island-West Cameron-East Breaks area of the continental sh

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Seismic Facies of Slope Basin Turbidite Reservoirs, East Breaks 160–161 Field: Pliocene-Pleistocene,rom four Pliocene to Pleistocene petroleum reservoirs interpreted as deep-water turbidite deposits. The oldest . reservoir is middle to late Pliocene and occurs about 80 km (50 miles) downslope from its age equivalent shelf/slope break. The youngest . A) reservoir is middle Pleistocene and occurs on

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Sequence Stratigraphy of the Oligocene Turbidite Complex of the Campos Basin, Offshore Brazil: An Ovshallow-marine siliciclastic sediments, previously stored in a pre-Oligocene subsiding area (Sao Tome Low), and the development of a distinct turbidite complex during the Oligocene..The Oligocene turbidite complex of Campos Basin consists of three main turbidite systems. They are genetically related

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Seismic Facies of Shelf, Slope, and Submarine Fan Environments of the Lewis Shale, Upper Cretaceous,ocument a vertical succession consisting of a condensed shelf shale overlain by bioturbated, probable turbidite sheet sandstone, deeper water sandy turbidites, and a progradational sandstone-shale interval of turbidite and deltaic deposits. Basin deepening and turbidite deposition were controlled by

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