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- W70376587 abstract "Thickness and sedimentation rates of time-stratigraphic units deposited during deltaic progradation can be predicted from a mathematical model. Depositional surfaces are constrained to lie along an assumed equilibrium bathymetric profile that advances seaward at a specified rate. Subsidence is treated as an isostatic response and so is related to the weight of accumulated sediment. Effects of contemporaneous compaction are included to obtain correct weights and thicknesses of stratigraphic units. For a uniformly prograding deltaic system with characteristics similar to that in the northern Gulf of Mexico, the model predicts that sedimentation rate at a fixed locality will continually increase as long as delta slope sediments are deposited. This is one of the reasons abnormally high fluid pressures and faults occur in offshore Louisiana." @default.
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- W70376587 date "1976-01-01" @default.
- W70376587 modified "2023-09-26" @default.
- W70376587 title "MATHEMATICAL MODELING OF SEDIMENT ACCUMULATION IN PROGRADING DELTAIC SYSTEMS" @default.
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- W70376587 doi "https://doi.org/10.1016/b978-0-08-020613-4.50015-x" @default.
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