Volume 46 Issue 3
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Article Navigation >  Earth Science  > 2021  >  46(3): 770-789
Sun Zhen, Li Fucheng, Lin Jian, Sun Longtao, Pang Xiong, Zheng Jinyun, 2021. The Rifting-Breakup Process of the Passive Continental Margin and Its Relationship with Magmatism: The Attribution of the South China Sea. Earth Science, 46(3): 770-789. doi: 10.3799/dqkx.2020.371
Citation: Sun Zhen, Li Fucheng, Lin Jian, Sun Longtao, Pang Xiong, Zheng Jinyun, 2021. The Rifting-Breakup Process of the Passive Continental Margin and Its Relationship with Magmatism: The Attribution of the South China Sea. Earth Science, 46(3): 770-789. doi: 10.3799/dqkx.2020.371
shu

The Rifting-Breakup Process of the Passive Continental Margin and Its Relationship with Magmatism: The Attribution of the South China Sea

doi: 10.3799/dqkx.2020.371
  • 1.

    Key Laboratory of Ocean and Marginal Sea Geology, South China Sea Institute of Oceanology, Innovation Academy of South China Sea Ecology and Environmental Engineering, Chinese Academy of Sciences, Guangzhou 511458, China

  • 2.

    Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou 511458, China

  • 3.

    China-Pakistan Joint Research Center for Earth Sciences, Islamabad 45320, Pakistan

  • 4.

    Laboratory for Marine Mineral Resources, Pilot National Laboratory for Marine Science and Technology, Qingdao 266237, China

  • 5.

    CNOOC Deepwater Development Limited, Shenzhen 518054, China

  • Received Date: 2020-11-15
  • Publish Date: 2021-03-01
    Abstract
  • Magma plays a key role in the rifting and breakup process of passive continental margin. Up to 10 km thick high velocity lower crust (HVLC) developed in the northeastern margin. Long term controversy toward its formation mechanism makes the margin classification difficult. In order to analyze the rifting and breakup mechanism of the SCS conjugate margins, this paper reviews the recent research progress of global margins, based on which the crustal structure and magmatic activity of the SCS are summarized. It is concluded that large amounts of magmatic activity occurred in the SCS with discrepancy between the eastern and western margins. The HVLC is thicker in the east and thinner or even absent in the west. It is speculated that the HVLC is of syn-rift underplating. According to the crustal structure and the amount of underplated magma, we suggest that the passive continental margin can be divided into 5 subclasses. The eastern continental margin of the SCS is of magma-robust type, and the middle and western margins are of magma-intermediate and magma-deficient types, respectively.In addition to the stretching rate, plate-edge rifting in the east and plate-interior rifting in the west continental margin may also contribute to the large difference in the amount of magmatic underplating.

     

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