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2020 Vol. 47, No. 5
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WANG Zhongbo, ZHANG Jiangyong, MEI Xi, CHEN Xiaohui, ZHAO Li, ZHANG Yong, ZHANG Zhixun, LI Xuejie, LI Rihui, LU Kai, SUN Rongtao, YANG Shouye. 2020. The stratigraphy and depositional environments of China' s sea shelves since MIS5(74-128)ka[J]. Geology in China, 47(5): 1370-1394. doi: 10.12029/gc20200506
Citation: WANG Zhongbo, ZHANG Jiangyong, MEI Xi, CHEN Xiaohui, ZHAO Li, ZHANG Yong, ZHANG Zhixun, LI Xuejie, LI Rihui, LU Kai, SUN Rongtao, YANG Shouye. 2020. The stratigraphy and depositional environments of China' s sea shelves since MIS5(74-128)ka[J]. Geology in China, 47(5): 1370-1394. doi: 10.12029/gc20200506
shu

The stratigraphy and depositional environments of China' s sea shelves since MIS5(74-128)ka

  • 1.

    Key Laboratory of Gas Hydrate, Ministry of Natural Resources, Qingdao Institute of Marine Geology, Qingdao 266071, Shandong, China

  • 2.

    Laboratory for Marine Mineral Resources, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266071, Shandong, China

  • 3.

    Guangzhou Marine Geological Survey, Guangzhou 510075, Guangdong, China

  • 4.

    School of Resources and Environmental Engineering, Shandong University of Technology, Zibo 255049, Shandong, China

  • 5.

    State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092, China

    • Fund Project: Supported jointly by Geological Survey Project of China Geological Survey (No. DD20160137, No. DD20160138,No. DD20190208, No. GZH201400201) and National Natural Science Foundation of China (No. 41876059,No. 41706069).
More Information
  • Author Bio: WANG Zhongbo, male, born in 1979, doctor, senior engineer, mainly engages in marine geology and Quaternary geology;E-mail:wangzhongbo@mail.cgs.gov.cn.
Received Date:  18 April 2020
Revised Date:  16 July 2020
Publish Date:  25 October 2020
    Abstract

  • Based on the comprehensive analysis of 28 boreholes of late Quaternary sedimentation and the high-resolution seismic profiles, the authors studied the stratigraphic characteristics identification and sedimentary environment rebuilding by comparing the results of other 46 boreholes as references in China's sea shelves. Three distinct transgression processes were discovered in the shelves of China's sea areas, with 3 marine strata well preserved. The strata of MIS1 and MIS3 are relatively thin in the Bohai Sea and the East China Sea, but thick in the Yellow Sea. There exists little sedimentation of Last Glacial period in the Bohai Sea and the Yellow Sea, but there have been quite integrated sedimentation units without obvious hiatus in the East China Sea since 100 ka B.P.. There were coastal and continental deposits in the inner shelf and nearshore and neritic deposition in the outer shelf of the South China Sea during late Pleistocene, with neritic sedimentation in Holocene. As a whole, the sedimentary environment changes of China's sea shelves since MIS5 in turn primarily were neritic and offshore deposits in MIS5 (74-128 ka), continental sedimentation of lagoon-fuvial-coast in MIS4 (60-74 ka), neritic and tidal flat deposits in MIS3 (24-60 ka), terrestrial or fluvial sedimentation in MIS2 (12-24 ka), and tidal sand ridge and neritic deposition in Holocene. Furthermore; the neotectonic movement and regional subsidence also influenced the late Quaternary stratigraphic development and their preservation in China seas. The results will provide direct evidence for the study of China's Quaternary sedimentation and global climate changes

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