南海北部陆缘结构及构造-岩浆演化

张翠梅; 孙珍; 赵明辉; 庞雄; ManatschalGianreto

doi:10.3799/dqkx.2021.208

Volume 47 Issue 7

Jul. 2022

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Zhang Cuimei, Sun Zhen, Zhao Minghui, Pang Xiong, Manatschal Gianreto, 2022. Crustal Structure and Tectono-Magmatic Evolution of Northern South China Sea. Earth Science, 47(7): 2337-2353. doi: 10.3799/dqkx.2021.208

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Zhang Cuimei, Sun Zhen, Zhao Minghui, Pang Xiong, Manatschal Gianreto, 2022. Crustal Structure and Tectono-Magmatic Evolution of Northern South China Sea. Earth Science, 47(7): 2337-2353. doi: 10.3799/dqkx.2021.208

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Crustal Structure and Tectono-Magmatic Evolution of Northern South China Sea

doi: 10.3799/dqkx.2021.208

Zhang Cuimei^{1, 2
,
,},
Sun Zhen^{1, 2
,
,
,},
Zhao Minghui^{1, 2},
Pang Xiong³,
Manatschal Gianreto⁴

1.
Key Laboratory of Ocean and Marginal Sea Geology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 511458, China
2.
Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou 511458, China
3.
Shenzhen Branch of China National Offshore Oil Corporation Limited, Shenzhen 518054, China
4.
Université de Strasbourg, CNRS, ITES UMR 7063, Strasbourg F-67084, France

Received Date: 2021-09-30
Publish Date: 2022-07-25

Abstract

Abstract

The northern continental margin of the South China Sea (SCS) developed a diagnostic crustal structure in the distal domain, which is characterized by "wide rift, thick basement, and prominent topographic variations of the top basement". These characteristics are significantly different from those of the typical magma-poor and magma-rich rifted margins. In order to decipher the origin of such crustal structure in the northern SCS, in this study it defines the nature of the basement in the distal margin based on the latest research progresses and the drilling results of the International Ocean Discovery Program (IODP), and discusses the detachment faults, magmatic additions and the tectono-magmatic interaction. The results suggest that several large-scale core complex structures were developed in the northern SCS during the early rifting (before 38 Ma), which was accompanied by voluminous magma intruding into the mid-lower crust. On the one hand, the emplacement of the syn-rift magma enhanced the ductile deformation of the mid-lower crust, resulting in the delocalization of the strain and the occurrence of the detachment in many places almost at the same time. On the other hand, the magmatism strongly affected the geometries of the detachment faults, resulting in the thickened basement. Finally, the syn-rift magmatism and the ductile flow of mid-lower crust are considered as the key factors to produce the wide rift in the northern SCS. The results would help to deepen the understanding of the crustal structure, deformation process and lithospheric thinning mechanism during the development of the rifted margins.
- crustal structure,
- detachment fault,
- magmatic evolution,
- core complex structure,
- rifted margin,
- South China Sea,
- marine geology

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References(96)

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Crustal Structure and Tectono-Magmatic Evolution of Northern South China Sea

doi: 10.3799/dqkx.2021.208

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