南海西南次海盆两侧陆缘中生代晚期构造接触关系

朱荣伟; 姚永坚; 刘海龄; 徐子英; 聂鑫; 杜文波

doi:10.3799/dqkx.2020.369

Volume 46 Issue 3

Mar. 2021

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Article Navigation > Earth Science > 2021 > 46(3): 885-898

Zhu Rongwei, Yao Yongjian, Liu hailing, Xu Ziying, Nie Xin, Du Wenbo, 2021. Tectonic Contact Relationship of Continental Margins of the Southwest Sub-Basin, South China Sea in Late Mesozoic. Earth Science, 46(3): 885-898. doi: 10.3799/dqkx.2020.369

Citation:

Zhu Rongwei, Yao Yongjian, Liu hailing, Xu Ziying, Nie Xin, Du Wenbo, 2021. Tectonic Contact Relationship of Continental Margins of the Southwest Sub-Basin, South China Sea in Late Mesozoic. Earth Science, 46(3): 885-898. doi: 10.3799/dqkx.2020.369

Citation:

Zhu Rongwei, Yao Yongjian, Liu hailing, Xu Ziying, Nie Xin, Du Wenbo, 2021. Tectonic Contact Relationship of Continental Margins of the Southwest Sub-Basin, South China Sea in Late Mesozoic. Earth Science, 46(3): 885-898. doi: 10.3799/dqkx.2020.369

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Tectonic Contact Relationship of Continental Margins of the Southwest Sub-Basin, South China Sea in Late Mesozoic

doi: 10.3799/dqkx.2020.369

Zhu Rongwei^{1, 2, 3
,
,},
Yao Yongjian^{1, 2
,
,},
Liu hailing³,
Xu Ziying^{1, 2},
Nie Xin^{1, 2},
Du Wenbo^{1, 2}

1.
Key Laboratory of Marine Mineral Resources, Ministry of Natural Resources, Guangzhou Marine Geological Survey, Guangzhou 510075, China
2.
Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou 511458, China
3.
CAS Key Laboratory of Ocean and Marginal Sea Geology, South China Sea Institute of Oceanology, Chinese Academy of Science, Guangzhou 511458, China

Received Date: 2020-11-25
Publish Date: 2021-03-15

Abstract

Abstract

In order to study the tectonic contact relationship of continental margins of the southwest sub-basin, South China Sea in the Late Mesozoic, and its influence on the formation and evolution of the South China Sea, this paper analyzes the crustal structure and Pre-Cenozoic structural deformation of the continental margins of the southwest sub-basin of the South China Sea by the geophysical data and the published data collected from continental margins of the southwest sub-basin. The crust structure and material composition of the continental margins of the southwest sub-basin are different, belonging to two micro blocks with different properties. The Pre-Cenozoic strata of continental margins of the southwest sub-basin experienced compression from different directions in the Late Mesozoic, and suffered uplift and denudation. The continental margins of the southwestern sub-basin were stitched together in the form of subduction collisions in the Late Mesozoic. The subduction zone is the extension of the northern South China Sea subduction zone to the southwest of the South China Sea. The expansion of the South China Sea in Cenozoic is related to the subduction zone, which is the initial fracture site of the South China Sea basin.
- Late Mesozoic,
- tectonic contact relationship,
- subduction and collision,
- southwestern sub-basin,
- South China Sea,
- marine geology

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Tectonic Contact Relationship of Continental Margins of the Southwest Sub-Basin, South China Sea in Late Mesozoic

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