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Very large subaqueous sand dunes on the upper continental slope in the South China Sea generated by episodic, shoaling deep-water internal solitary waves

Marine GeologyUpper Continental SlopeEarth ScienceEngineeringComplex Sea StateWave GroupSouth China SeaShallow Water HydrodynamicsOceanographyCoastal DepositSedimentologySediment TransportOcean Internal Wave