南海陆缘中南-礼乐断裂带的发育与构造活动

邱燕; 聂鑫; 阎贫; 黄文凯; 杜文波; 鞠东

doi:10.3799/dqkx.2023.146

Volume 49 Issue 10

Oct. 2024

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Article Navigation > Earth Science > 2024 > 49(10): 3471-3487

Qiu Yan, Nie Xin, Yan Pin, Huang Wenkai, Du Wenbo, Ju Dong, 2024. Zhongnan-Liyue Fault Zone Developed at Continental Margins of the South China Sea and Tectonic Movements. Earth Science, 49(10): 3471-3487. doi: 10.3799/dqkx.2023.146

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Qiu Yan, Nie Xin, Yan Pin, Huang Wenkai, Du Wenbo, Ju Dong, 2024. Zhongnan-Liyue Fault Zone Developed at Continental Margins of the South China Sea and Tectonic Movements. Earth Science, 49(10): 3471-3487. doi: 10.3799/dqkx.2023.146

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Zhongnan-Liyue Fault Zone Developed at Continental Margins of the South China Sea and Tectonic Movements

doi: 10.3799/dqkx.2023.146

Qiu Yan^{1, 2
,
,},
Nie Xin^{1, 2},
Yan Pin^{2, 3},
Huang Wenkai^{1, 2},
Du Wenbo^{1, 2},
Ju Dong^{1, 2}

1.
Key Laboratory of Marine Mineral Resources, Ministry of Natural Resources, Guangzhou Marine Geological Survey, Guangzhou 510075, China
2.
Key Laboratory of Ocean and Marginal Sea Geology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 511458, China
3.
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 510301, China

Received Date: 2022-12-04
Available Online: 2024-11-08
Publish Date: 2024-10-25

Abstract

Abstract

Whether a strike-slip fault zone of S-N trend developed in the centre South China Sea (SCS) has been focused by geologists who study tectonic evolution, but no any conclusion due to lack of data.The difficult issue has been resolved in this paper by studying the distribution of residual Mesozoic strata and interpreting new geological and geophysics data in the SCS. Zhongnan-Liyue (ZL) fault zone, a strike-slip fault zone with S-N trend, developed at both southern and northern continental margins and the initial time of its activity was at least in Mesozoic.Before sea-floor spreading of the SCS, this strike-slip fault zone attains about 700 km at southern and northern continental margins. In different geological times this fault zone was of different characteristics of tectonic movement, that was strike slip of left-rotation in Mesozoic, strike slip and extension in Early-Middle Paleogene, in order to strike slip in Late Paleogene and Early Neogene, last one strike slip accompanying pressure function in Middle-Late Neogene.
- Zhongnan-Liyue fault zone,
- residual Mesozoic strata,
- strike-slip fault with S-N trend,
- tectonic movement,
- east of continental margin of the SCS,
- marine geology

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References(57)

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Zhongnan-Liyue Fault Zone Developed at Continental Margins of the South China Sea and Tectonic Movements

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