(Q57550889)

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The significance of large sediment supply, active tectonism, and eustasy on margin sequence development: Late Quaternary stratigraphy and evolution of the Ganges–Brahmaputra delta

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The significance of large sediment supply, active tectonism, and eustasy on margin sequence development: Late Quaternary stratigraphy and evolution of the Ganges–Brahmaputra delta (English)

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author name string

S.L. Goodbred

1

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S.A. Kuehl

2

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publication date

June 2000

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Sedimentary Geology

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133

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227-248

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3-4

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Reef drowning during the last deglaciation: Evidence for catastrophic sea-level rise and ice-sheet collapse

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Relation of sequence stratigraphy to modern sedimentary environments

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Brahmaputra river: Channel processes and sedimentation

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A Large Drop in Atmospheric 14C/12C and Reduced Melting in the Younger Dryas, Documented with 230Th Ages of Corals.

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A 17,000-year glacio-eustatic sea level record: influence of glacial melting rates on the Younger Dryas event and deep-ocean circulation

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A 13,000-year climate record from western Tibet

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Floodplain processes in the Bengal Basin and the storage of Ganges–Brahmaputra river sediment: an accretion study using 137Cs and 210Pb geochronology

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Shelf sedimentation off the Ganges-Brahmaputra river system: Evidence for sediment bypassing to the Bengal fan

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Subaqueous delta of the Ganges-Brahmaputra river system

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Geomorphic/Tectonic Control of Sediment Discharge to the Ocean: The Importance of Small Mountainous Rivers

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Variability of deltaic processes in terms of sediment supply, with particular emphasis on grain size

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Worldwide initiation of holocene marine deltas by deceleration of sea-level rise

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Extended 14C Data Base and Revised CALIB 3.0 14C Age Calibration Program

1 reference

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Sediment transport and deposition at river mouths: A synthesis

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Identifiers

10.1016/S0037-0738(00)00041-5

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2000SedG..133..227G

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