Journal of Jilin University(Earth Science Edition) ›› 2019, Vol. 49 ›› Issue (1): 96-105.doi: 10.13278/j.cnki.jjuese.20180131

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Research Progress and Discussion on Formation and Tectonics of South Yellow Sea

Hou Fanghui1,2, Guo Xingwei1,2, Wu Zhiqiang1,2, Zhu Xiaoqing1,2, Zhang Xunhua2,3, Qi Jianghao1,2, Wang Baojun1,2, Wen Zhenhe1,2, Cai Laixing1,2, Pang Yumao1,2   

  1. 1. Qingdao Institute of Marine Geology, China Geological Survey, Qingdao 266071, Shandong, China;
    2. Laboratory for Marine Mineral Resources, Pilot National Laboratory for Marine Science and Technology(Qingdao), Qingdao 266071, Shandong, China;
    3. Nanjing Center, China Geological Survey, Nanjing 210016, China
  • Received:2018-05-25 Online:2019-01-26 Published:2019-01-18
  • Supported by:
    Supported by National Natural Science Foundation of China(41776081,41210005),Aoshan Technological Innovation Projects of National Laboratory for Marine Science and Technology(Qingdao)(2015ASKJ03), and National Marine Geology Special Project of China (DD20160147,DD20179393)

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Abstract: The South Yellow Sea basin is a multi-cycle basin with a sandwich-type construction on the pre-Sinian metamorphic basement of the lower Yangtze platform. The geologic evolution of the basin can be divided into three stages:the Sinian-Early Triassic marine basin, the Cretaceous-Paleogene graben fault basin and the Neogene-Quaternary depression basin stages. There are still a lot of debates on the stratigraphic framework and distribution characteristics of multistage basins, basin deformation and dynamics mechanism, basin property and genetic mechanism at present. In this paper, some problems about strata and tectonics in South Yellow Sea are discussed based on geological-geophysical data obtained in recent years,combined with the previous research. The comprehensive research shows that:There is no Indo-Early Yanshanian foreland basin under the fault depression basin since Late Yanshanian in the northern basin of South Yellow Sea. There is indeed a fault zone in the western edge of the Korean Peninsula. In the collision between the Yangtze block and the North China block, there were many multi-layer interwedging structures formed in the crust. The Mesozoic-Paleozoic marine strata are widely distributed in the South Yellow Sea and denuded eastward,and maybe only the lower Paleozoic remains. The whole Lower Triassic-Sinian strata remain in the Central Uplift.

Key words: formation, tectonic characteristics, composite basin, South Yellow Sea

CLC Number: 

  • P548
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