Spatial and temporal variations and controlling factors of sediment accumulation in the Yangtze River estuary and its adjacent sea area in the Holocene, especially in the Early Holocene
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文摘

We presented a transport and accumulation pattern of the Yangtze-derived sediment.

The Early Holocene strata scoured by the later tidal current formed the mud ridges.

The accumulation rates exhibit two trends, i.e., low-high-low, and high-low-high.

The position shifts of the estuary caused the changes in accumulation rate.

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