新疆乌孙山北缘断裂晚第四纪活动及区域构造意义

袁四化; 刘晓燕; 白相东; 李建刚; 迟宝明; 姜纪沂; 李瑛; 赵振宏

doi:10.3799/dqkx.2018.396

Volume 44 Issue 10

Nov. 2019

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Article Navigation > Earth Science > 2019 > 44(10): 3541-3550

Yuan Sihua, Liu Xiaoyan, Bai Xiangdong, Li Jiangang, Chi Baoming, Jiang Jiyi, Li Ying, Zhao Zhenhong, 2019. Constraints on Late Quaternary Activity of North Wusunshan Fault in Xinjiang and Its Regional Tectonic Implications. Earth Science, 44(10): 3541-3550. doi: 10.3799/dqkx.2018.396

Citation:

Yuan Sihua, Liu Xiaoyan, Bai Xiangdong, Li Jiangang, Chi Baoming, Jiang Jiyi, Li Ying, Zhao Zhenhong, 2019. Constraints on Late Quaternary Activity of North Wusunshan Fault in Xinjiang and Its Regional Tectonic Implications. Earth Science, 44(10): 3541-3550. doi: 10.3799/dqkx.2018.396

Citation:

Yuan Sihua, Liu Xiaoyan, Bai Xiangdong, Li Jiangang, Chi Baoming, Jiang Jiyi, Li Ying, Zhao Zhenhong, 2019. Constraints on Late Quaternary Activity of North Wusunshan Fault in Xinjiang and Its Regional Tectonic Implications. Earth Science, 44(10): 3541-3550. doi: 10.3799/dqkx.2018.396

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Constraints on Late Quaternary Activity of North Wusunshan Fault in Xinjiang and Its Regional Tectonic Implications

doi: 10.3799/dqkx.2018.396

1.
College of Earth Sciences, Institute of Disaster Prevention, Sanhe 065201, China
2.
Xi'an Center of Geological Survey, China Geological Survey, Xi'an 710054, China

Received Date: 2018-12-16
Publish Date: 2019-11-11

Abstract

Abstract

North Wusunshan fault zone lies on southern margin of Yining basin, Xinjiang, which is a boundary fault between Yining basin and Wusunshan. The fault zone is composed of a suit of secondary parallel or en echelon faults. The faults strike in east-west direction, and dip to the south generally, the main fault next to Wusunshan is characterized by steep reverse fault plane with dip angle of 50°-80°, the frontal fault close to Yining basin shows gentler fault plane. The Carboniferous and Permian strata consist of hanging wall, and the Quaternary and Jurassic strata make up the footwall. ESR dating of sediments for hanging wall and footwall indicates that the Mid-Upper Pleistocene is truncated by the faults in specific places. Based on stratigraphic contact and regional tectonic analysis, North Wusunshan faults thrust intensively toward the north during the latest Mid-Pleistocene, in the meanwhile, North Yining faults thrust intensively toward the south, and the two groups of fault belts control basin-mountain geomorphic framework. This tectonic event is equivalent with the Gonghe Movement in the Tibet plateau, which is attributed to compression from the North and South Tianshan, which thrust toward Yili basin, regional tectonic mechanism stemmed from outward growth and expansion of the Tibetan plateau.
- north Wusunshan fault,
- Yining basin,
- active tectonics,
- electron spin resonance (ESR) dating,
- tectonics

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Constraints on Late Quaternary Activity of North Wusunshan Fault in Xinjiang and Its Regional Tectonic Implications

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