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Sediment composition suggests a mixed provenance with sediment supplies from both orogenic belts and cratons.
Deposition dominated within the proglacial depression, with approximately 3.8∗107 m3 of sediment, and along channel systems that remained connected to subglacial sediment supplies.
The width-to-depth ratio, the slope change, the bend upstream of the reach, and the sediment supplies are the main controls of bar formation and evolution.
In order to better understand their relationships, detailed environmental facies, channel fairways, source directions of the sediment supplies, burial depth/history, and paleo-bathymetries have been rebuilt and mapped out using well, seismic and log data.
This unique submarine canyon in the Qiongdongnan Basin is suggested to be characterized by axial gravity flow, ascribing to different gravity deposits originated from different sediment supplies and the tectonic activities.
Small differences in the distribution and characteristics of the seismic units in each area are attributed to local factors, such as physiography of the coastal plains, the wave climate and increased sediment supplies conditioned by anthropic actions.
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Another important feature in sedimentation process is sediment supply.
This relationship between sedimentation and tectonics is sediment supply-driven.
This limits the rate of sediment supply to regulated reaches.
Sediment supply by fluvial sources gave way in the Pleistocene to direct glacial sediment supply to the slope.
Not surprisingly, they conclude that deltas are "highly sensitive" to the balance between sediment supply and wave energy.
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