南海构造变形分区及成盆过程

雷超; 任建业; 张静

doi:10.3799/dqkx.2015.062

Volume 40 Issue 4

Apr. 2015

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Lei Chao, Ren Jianye, Zhang Jing, 2015. Tectonic Province Divisions in the South China Sea: Implications for Basin Geodynamics. Earth Science, 40(4): 744-762. doi: 10.3799/dqkx.2015.062

Citation:

Lei Chao, Ren Jianye, Zhang Jing, 2015. Tectonic Province Divisions in the South China Sea: Implications for Basin Geodynamics. Earth Science, 40(4): 744-762. doi: 10.3799/dqkx.2015.062

Lei Chao, Ren Jianye, Zhang Jing, 2015. Tectonic Province Divisions in the South China Sea: Implications for Basin Geodynamics. Earth Science, 40(4): 744-762. doi: 10.3799/dqkx.2015.062

Citation:

Lei Chao, Ren Jianye, Zhang Jing, 2015. Tectonic Province Divisions in the South China Sea: Implications for Basin Geodynamics. Earth Science, 40(4): 744-762. doi: 10.3799/dqkx.2015.062

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Tectonic Province Divisions in the South China Sea: Implications for Basin Geodynamics

doi: 10.3799/dqkx.2015.062

Lei Chao^{1, 2
,},
Ren Jianye^{1, 2},
Zhang Jing^{1, 2}

1.
Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education, China University of Geosciences, Wuhan 430074, China
2.
Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China

Received Date: 2014-08-11
Publish Date: 2015-04-01

Abstract

Abstract

In order to better understand the evolution and mechanism of Cenozoic sedimentary basins in the South China Sea, we employed tectono-stratigraphic analysis on the sedimentary basins in the South China Sea. Reviewing the previous studies on the tectonics and sedimentation in the South China Sea and its peripheral regions, we used a compilation of newly acquisition and reprocessed seismic reflection profiles covering the large basins and got a clear result of the basins in the South China Sea with different basin structures, evolutions and mechanism. Considering the nature of the basin developed in the South China Sea, we suggested in our paper that the basins in the South China Sea can be divided into two sedimentary basin groups by a tectonic boundary, which is characterized by a transform boundary of the Red River fault extended south along the Vietnamese margin and joined with the trench along the Lupar line. These two basin groups are collsion-extrusion tectonic province basin group and Proto-South China Sea slab pull tectonic province basin group. The Proto-South China Sea tectonic province basin group is strongly controlled by the southward subduction of Proto-South China Sea. These basins include Beibuwan, Qiongdongnan, Pearl River Mouth, Zengmu, Beikang, Brunei-Sabah, Liyue basins and so on.However, the evolution of the collision-extrusion tectonic province basin group is controlled by the extrusion toward the southeast and rotation of Indochina block, which is as a result of the indentation of rigid India into Asia. This kind of basins mainly includes Yinggehai, Zhongjiannan, Mekong, Wan'an basins and so on. Considering the peripheral plate dynamic events, the tectonics of these basins and significant boundaries refined on the seismic profiles, the evolution of the South China Sea and its peripheral regions is reconstructed in our paper.
- the South China Sea,
- tectonic revolutionary boundary,
- Proto-South China Sea,
- collision-extrusion tectonics,
- marine geology

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References(103)

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Tectonic Province Divisions in the South China Sea: Implications for Basin Geodynamics

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