Deep-water bottom current evolution in the northern South China Sea during the last 150 kyr: Evidence from sortable-silt grain size and sedimentary magnetic fabric

Journal of Asian Earth Sciences(2019)

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摘要
•Magnetic fabric and grain size properties are used to reconstruct the bottom current.•The increased deep water bottom current corresponds to Heinrich Stadials.•The evolution of bottom current is closely related to the global climate.
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关键词
Deep-water bottom current,Magnetic susceptibility anisotropy,Sortable silt,Heinrich stadials,South China Sea
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