准噶尔盆地西北缘哈山构造带断裂性质与演化

巴素玉; 李长圣; 汪伟; 宋亮; 谷今; 卢宁; 池禹; 张新松; 朱素芹; 张勇

doi:10.3799/dqkx.2025.298

Volume 51 Issue 5

May 2026

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Ba Suyu, Li Changsheng, Wang Wei, Song Liang, Gu Jin, Lu Ning, Chi Yu, Zhang Xinsong, Zhu Suqin, Zhang Yong, 2026. Fault System and Evolution Process of Hashan Structural Belt in Northwestern Junggar Basin. Earth Science, 51(5): 1893-1907. doi: 10.3799/dqkx.2025.298

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Ba Suyu, Li Changsheng, Wang Wei, Song Liang, Gu Jin, Lu Ning, Chi Yu, Zhang Xinsong, Zhu Suqin, Zhang Yong, 2026. Fault System and Evolution Process of Hashan Structural Belt in Northwestern Junggar Basin. Earth Science, 51(5): 1893-1907. doi: 10.3799/dqkx.2025.298

Citation:

Ba Suyu, Li Changsheng, Wang Wei, Song Liang, Gu Jin, Lu Ning, Chi Yu, Zhang Xinsong, Zhu Suqin, Zhang Yong, 2026. Fault System and Evolution Process of Hashan Structural Belt in Northwestern Junggar Basin. Earth Science, 51(5): 1893-1907. doi: 10.3799/dqkx.2025.298

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Fault System and Evolution Process of Hashan Structural Belt in Northwestern Junggar Basin

doi: 10.3799/dqkx.2025.298

Ba Suyu^{1
,
,},
Li Changsheng²,
Wang Wei^{3
,
,
,},
Song Liang¹,
Gu Jin¹,
Lu Ning¹,
Chi Yu²,
Zhang Xinsong²,
Zhu Suqin²,
Zhang Yong³

1.
Geophysical Research Institute, Shengli Oilfield Company, SINOPEC, Dongying 257022, China
2.
School of Earth and Planetary Sciences, East China University of Technology, Nanchang 330013, China
3.
State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China

Received Date: 2025-08-20
Publish Date: 2026-05-25

Abstract

Abstract

The fault property of the Hashan structural belt, located in the southwestern Junggar basin, is still controversial. In this paper it constructs the structural model of the Hashan structural belt by interpreting the latest seismic profile, and analyzes the fault displacements. The evolution process is investigated using balanced cross-section restoration. The results suggest that the Hashan structural belt is a complex fault system undergoing multiple stages of deformation. The Darabut fault system forms a typical flower structure controlled by the basement-involved strike-slip fault, and the Wuerhe-Xiazijie fault system develops a thrust deformation as the compressional stress propagates toward the Junggar basin. The Hashan structural belt has experienced three deformation stages since the Permian. The Darabut fault system predominantly formed in the Late Permian. The Wuerhe-Xiazijie fault system formed during the deformation from the Triassic to the Jurassic, and the Hashan structural belt kept lifting from the Cretaceous to the Cenozoic.
- earthquake,
- strike-slip fault,
- fault displacement,
- Hashan structural belt,
- Junggar basin,
- tectonics

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References(53)

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Fault System and Evolution Process of Hashan Structural Belt in Northwestern Junggar Basin

doi: 10.3799/dqkx.2025.298

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