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Types of slope belts, subsidence rate, sediment provenance and their evolution jointly control the sediment-dispersal characters in deposition area.
Two primary ways to control the sediment pouring into the Yellow River from this area are planting and engineering measures.
(2) The base-level changes that control the sediment infilling of incised meandering valleys have not yet been extensively investigated in a rejuvenated foreland basin.
We can also assess how the major element compositions compare with one another to assess the processes that control the sediment composition.
Model simulations where distributary length affects sediment discharge demonstrate how the dynamics of one distributary can control the sediment discharge of another.
The data also provide evidence showing that organic matter is the key-parameter in Cu concentration control in the sediments through burial and accumulation processes especially in the swamp area.
The hinterland tectonism as well as the climate controls the sediment supply.
In addition, major tectonic elements controlling the sediment depositional patterns within the basin have also been examined.
The record of turbidite events in these cores is interpreted in terms of volcanic and climatic changes that could have controlled the sediment transfer to the deep ocean.
Folding controlled the sediment distribution during most of the Neogene strata, while the normal faulting of the anticlines represent basin potential for hydrocarbon.
However, during the tectonic quiescence or rift-depression transition stage, significant changes of climate would play a primary role in controlling the sediment dispersal.
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