Controls on turbidite sedimentation: Insights from a quantitative approach of submarine channel and lobe architecture (Late Quaternary Congo Fan)
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文摘

Exhaustive architectural evolution of the Congo turbidite system since 200 ka.

Shifts of channel-levee-lobe systems reveal cyclic patterns at different time scales.

Dimensions of terminal lobe complexes do not exhibit cyclic evolution.

Pointing to permanent internal control by inherited topography.

Revealing possible exceptional periods of increased or coarsening Congo River inputs.

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