Middle Miocene reworked turbidites in the Baiyun Sag of the Pearl River Mouth Basin, northern South China Sea margin: Processes, genesis, and implications
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文摘

Ancient reworked turbidites are recognized.

Reworked turbidites were created by turbidity and contour flows and internal tides.

Reworked turbidites are characterized by traction structures and tidal signatures.

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