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- W2371960170 abstract "The composition characteristic of the clay mineral in the core SYDP103 is most of the samples consisted of illite, chlorite, kaolinite and montmorillonite, which are sourced from the redeposite of the clay mineral in the Changjiang River, surrounding terreginous materials in origin and neighbouring sea areas. The dominate dynamic is eddying motion for sediment environment of the clay mineral in the study area.The distribution characteristic and change in content of this core SYDP103 have distinct corresponding relationship with spore assemblages from the last glacial stage. It was reflected that the climate characteristic determines the composition of clay mineral, which is coincident with four climatic stages of global(Boreal period, Atlantic period, Sub-Boreal period,Sub-Atlantic period) in the Holocene." @default.
- W2371960170 created "2016-06-24" @default.
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- W2371960170 date "2007-01-01" @default.
- W2371960170 modified "2023-09-23" @default.
- W2371960170 title "Clay mineral composition and palaeoclimate signification of the core SYDP103 in the Yellow Sea" @default.
- W2371960170 hasPublicationYear "2007" @default.
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