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    Volume 45 Issue 7
    Jul.  2020
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    Wang Zhongbo, Lu Kai, Wen Zhenhe, Zhang Zhixun, Li Rihui, Mei Xi, Lan Xianhong, 2020. Grain Size Compositions and Their Influencing Factors of the Surface Sediments in Eastern China Seas. Earth Science, 45(7): 2709-2721. doi: 10.3799/dqkx.2020.028
    Citation: Wang Zhongbo, Lu Kai, Wen Zhenhe, Zhang Zhixun, Li Rihui, Mei Xi, Lan Xianhong, 2020. Grain Size Compositions and Their Influencing Factors of the Surface Sediments in Eastern China Seas. Earth Science, 45(7): 2709-2721. doi: 10.3799/dqkx.2020.028

    Grain Size Compositions and Their Influencing Factors of the Surface Sediments in Eastern China Seas

    doi: 10.3799/dqkx.2020.028
    • Received Date: 2020-02-18
    • Publish Date: 2020-07-15
    • Based on 1 438 grain size data obtained by marine regional geologic survey, surface sediments of the eastern China Seas are divided into seven types including sandy silt, silty sand, silt, sand, sandy mud, muddy sand and mud by Folk nomenclature.Meanwhile, the grain size features and their parameters are well described.Among them, sandy silt, silty sand, and silty sand are the three main sediment types, accounting for 34.70%, 24.20% and 15.51% respectively.The distribution of silty sand is strip-shaped in the south area.Silty sand is mainly distributed in Zhejiang and Fujian coastal zones, the western Bohai Sea, the central and northern areas of the southern Yellow Sea.Sand is mainly distributed on the East China Sea shelf, Yangtze Shoal, Subei Shoal and western Korea Bay.The influence factors of the sediments distribution include provenance, hydrodynamic environment, water depth, topography and geomorphology, etc. The sea level changes and ocean circulations during the Late Quaternary control the sediment flux into the seas and the sedimentary system on the shelves.Based on the dynamic properties of Folk classification and the type distributions, four kind of sedimentary areas are mainly identified in the eastern China Seas, such as estuarine deposition areas, shelf muddy deposition areas, tidal deposition areas and residual deposition areas.The formation mechanism and influence factors of different sedimentary areas are significantly different, which reflects the process of clastic sediment migration with the sea level changes affected by the special topography of the eastern China Seas.

       

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