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Event-driven deltaic sedimentation on a low-gradient, low-energy shelf: The Brazos River subaqueous delta, northwestern Gulf of Mexico
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Sediment accumulated from flood events and reworked proximal shelf sediments

The depocenter migrated over time due to changes in the fluvial sediment supply

Current event beds can be completely remobilized within a year of deposition

Study shows delta accumulation through fluvial and marine-derived sediment inputs

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