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Scour in large braided rivers and the recognition of sequence stratigraphic boundaries
J.L. Best
, Philip Ashworth
University of Brighton
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Keyphrases
Braided River
100%
Base Level
100%
Channel Depth
100%
Sequence Stratigraphic
100%
Stratigraphic Boundaries
100%
Bangladesh
50%
Jamuna River
50%
Sedimentary Sequence
50%
Channel Confluence
50%
Ancient Sediments
50%
Sea-level Change
50%
Incision
50%
Erosion Surface
50%
Basal Erosion
50%
Channel Bend
50%
Shallow Marine Sediments
50%
Floodplain Width
50%
Bed Scour
50%
Earth and Planetary Sciences
Braided River
100%
Sea Level
100%
Stratigraphic Boundary
100%
Sedimentary Sequence
50%
Flood Plain
50%
Marine Sediment
50%
Sea Level Change
50%
Bangladesh
50%