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SHANG Luning, ZHANG Yong, YAO Yongjian, WU Hao, HU Gang, TIAN Zhixian. 2020. Late Cenozoic evolution of East China continental margin and restoration of plate interaction processes[J]. Geology in China, 47(5): 1323-1336. doi: 10.12029/gc20200503
Citation: SHANG Luning, ZHANG Yong, YAO Yongjian, WU Hao, HU Gang, TIAN Zhixian. 2020. Late Cenozoic evolution of East China continental margin and restoration of plate interaction processes[J]. Geology in China, 47(5): 1323-1336. doi: 10.12029/gc20200503
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Late Cenozoic evolution of East China continental margin and restoration of plate interaction processes

  • 1.

    Qingdao Institute of Marine Geology, Qingdao 266071, Shandong, China

  • 2.

    Guangzhou Marine Geological Survey, Guangzhou 510075, Guangdong, China

    • Fund Project: Supported by Geological Survey Project (No. DD20160137, No. DD20160138, No. DD20190236) and National Natural Science Foundation of China (No. 41606050).
More Information
  • Author Bio: SHANG Luning, male, born in 1986, associate researcher, mainly engages in the study of marine tectonics; E-mail:shang1924@163.com
  • Corresponding author: ZHANG Yong, male, born in 1970, senior researcher, mainly engages in marine regional geological survey and research; E-mail:qimgzy@163.com  
Received Date:  03 April 2020
Revised Date:  05 August 2020
Publish Date:  25 October 2020
    Abstract

  • The tectonic activities of the continental margin of eastern China during the Late Cenozoic were mainly concentrated on the eastern margin of the East China Sea. Since the Miocene, a series of major tectonic processes, such as the subduction of the Philippine plate, the back-arc rifting of the Okinawa Trough and the Taiwan arc-continent collision, have shaped the present tectonic-geomorphological patterns of the Ryukyu trench-arc-back-arc basin system, the Taiwan collision orogenic belt and the northeastern South China Sea. Based on the interpretation of gravity, magnetism and multi-channel seismic data and combined with previous research results, the authors restored the tectonic evolution history of the Okinawa Trough and clarified the relationship between the back-arc tension of the Okinawa Trough and the Taiwan arc-land collision. On such a basis, the interaction processes between the Eurasian plate, the Philippine Sea plate and the South China Sea plate since Miocene were reconstructed, and a new model of plate interaction was proposed. This work is helpful to the further understanding of the constraints and effects of deep dynamic and thermal processes on shallow tectonic framework changes in the context of plate convergence on the East Asian continental margin.

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