库车坳陷西段阿瓦特构造转换带盐构造演化特征及影响因素

吴珍云; 杨秀磊; 尹宏伟; 董少春; 李长圣; 汪伟; 贾东

doi:10.3799/dqkx.2022.312

Volume 48 Issue 4

Apr. 2023

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Article Navigation > Earth Science > 2023 > 48(4): 1271-1287

Wu Zhenyun, Yang Xiulei, Yin Hongwei, Dong Shaochun, Li Changsheng, Wang Wei, Jia Dong, 2023. Characteristics and Influencing Factors of Salt Structure Evolution in Awate Transfer Zone, Western Kuqa Depression. Earth Science, 48(4): 1271-1287. doi: 10.3799/dqkx.2022.312

Citation:

Wu Zhenyun, Yang Xiulei, Yin Hongwei, Dong Shaochun, Li Changsheng, Wang Wei, Jia Dong, 2023. Characteristics and Influencing Factors of Salt Structure Evolution in Awate Transfer Zone, Western Kuqa Depression. Earth Science, 48(4): 1271-1287. doi: 10.3799/dqkx.2022.312

Citation:

Wu Zhenyun, Yang Xiulei, Yin Hongwei, Dong Shaochun, Li Changsheng, Wang Wei, Jia Dong, 2023. Characteristics and Influencing Factors of Salt Structure Evolution in Awate Transfer Zone, Western Kuqa Depression. Earth Science, 48(4): 1271-1287. doi: 10.3799/dqkx.2022.312

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Characteristics and Influencing Factors of Salt Structure Evolution in Awate Transfer Zone, Western Kuqa Depression

doi: 10.3799/dqkx.2022.312

Wu Zhenyun^{1, 2
,
,},
Yang Xiulei^{1, 2},
Yin Hongwei³,
Dong Shaochun³,
Li Changsheng^{1, 2},
Wang Wei³,
Jia Dong³

1.
State Key Laboratory of Nuclear Resources and Environment, East China University of Technology, Nanchang 330013, China
2.
School of Earth Sciences, East China University of Technology, Nanchang 330013, China
3.
School of Earth Sciences and Engineering, Nanjing University, Nanjing 210046, China

Received Date: 2022-06-06
Publish Date: 2023-04-25

Abstract

Abstract

In order to determine the characteristics and influencing factors of salt structure evolution located at the border of salt basin in western Kuqa depression, a comprehensive analysis of Awate transfer zone was carried out by field geological survey, structural analysis of industrial seismic profiles and 3D sand-box analogue modeling experiment. The results show follows. (1)Awate structural belt is a typical compressional structural transfer zone in western Kuqa depression, where differential structures formed from imbricated thrust faults in the Wushi sag to salt-related folds in the Awate sag. (2) The Talake strike-slip fault occurred at the junction of Wushi sag and Awate sag is an accommodative transverse fault developed in the overburden. Influenced by this fault, Talake syncline, Talake anticline and other drag salt-related structures formed in the overburden. The closer to the Talake strike-slip fault, the stronger the drag and wrinkling effect becomes, and even the fold-related faults are easy to develop, prompting the outcrop of salt rock in the core of anticline. (3) The Cenozoic deformation of Awate structural transfer zone is mainly controlled by regional compression, the distribution of salt rock and the activity of basement faults.
- Kuqa depression,
- Awate structural transfer zone,
- salt-related fold,
- Talake strike-slip fault,
- sand-box analogue modeling,
- structural geology

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References(66)

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Characteristics and Influencing Factors of Salt Structure Evolution in Awate Transfer Zone, Western Kuqa Depression

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