Morphobathymetric analysis of the large fine-grained sediment waves over the Gulf of Valencia continental slope (NW Mediterranean)
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文摘

Large sediment waves are developed over the Gulf of Valencia continental slope.

Wavelengths of 500–1000 m and maximum wave heights of 50 m are observed.

Near-inertial internal waves are proposed as the generation mechanism.

The continental slope gradient determines the sediment waves' shape and evolution.

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