Red River Fault Zone affected the formation of basins in the western South China Sea: An experimental study

ZHANG Jiaxuan; GUO Lingli; ZHANG Jingjing; TAO Wei; ZHAO Shujuan; WANG Guangzeng; LI Sanzhong

doi:10.16562/j.cnki.0256-1492.2024020101

2025 Vol. 45, No. 2

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Article navigation > Marine Geology & Quaternary Geology > 2025 > 45(2): 79-97

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ZHANG Jiaxuan, GUO Lingli, ZHANG Jingjing, TAO Wei, ZHAO Shujuan, WANG Guangzeng, LI Sanzhong. Red River Fault Zone affected the formation of basins in the western South China Sea: An experimental study[J]. Marine Geology & Quaternary Geology, 2025, 45(2): 79-97. doi: 10.16562/j.cnki.0256-1492.2024020101

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ZHANG Jiaxuan, GUO Lingli, ZHANG Jingjing, TAO Wei, ZHAO Shujuan, WANG Guangzeng, LI Sanzhong. Red River Fault Zone affected the formation of basins in the western South China Sea: An experimental study[J]. Marine Geology & Quaternary Geology, 2025, 45(2): 79-97. doi: 10.16562/j.cnki.0256-1492.2024020101

Red River Fault Zone affected the formation of basins in the western South China Sea: An experimental study

1.
Frontiers Science Center for Deep Ocean Multispheres and Earth System, Key Lab of Submarine Geosciences and Prospecting Techniques, MOE, College of Marine Geosciences, Ocean University of China, Qingdao 266100, China
2.
Laboratory for Marine Mineral Resources, Qingdao Marine Science and Technology Center, Qingdao 266237, China

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Corresponding author: GUO Lingli, guolingli@ouc.edu.cn

Received Date: 01 February 2024

Revised Date: 11 March 2024

Accepted Date: 11 March 2024

Publish Date: 28 April 2025

Abstract

Abstract

The strike-slip movement of the Red River Fault Zone (RRFZ) affected the formation of the basin in the western part of the South China Sea (SCS) to a certain degree. To characterize the tectonic features of the RRFZ during the uplift interval of the Tibetan Plateau and analyze the relationship between the strike-slip in RRFZ and the basins, especially Yinggehai Basin and Zhongjiannan Basin in the western SCS, sandbox analogue modelling experiments were performed in the context of the India-Eurasia collision. Results indicate that the prototypes of the two basins are controlled by the NW-oriented shear stresses generated by the strike-slip movement of the RRFZ, and the SN-oriented tensional stresses with the SCS opening up and the basin sizes expanding. During the early formation stage of the two basins, the displacement due to the strike-slipping was absorbed by the boundary faults and internal faults of the basins, thus controlling the evolution of the basins during the stage from 35 to 23 Ma.
- analogue modelling /
- basin formation dynamic /
- Red River Fault Zone /
- Yinggehai Basin /
- Zhongjiannan Basin

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References

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