Failure mechanics, transport behavior, and morphology of submarine landslides
Submarine landslides retrogressively fail from intact material at the headwall and then become fluidized by strain weakening; the final deposits of these flows have low porosity, which controls their character in seismic reflection data. Submarine landslides occur on the open slope and also localize...
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Format: | Others |
Language: | English |
Published: |
2012
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Online Access: | http://hdl.handle.net/2152/ETD-UT-2010-12-2518 |