铲式逆冲断层的地貌约束：以东天山尤路都斯盆地巴音背斜构造为例

武登云; 任治坤; 吕红华; 刘金瑞; 雷惊昊; 包国栋; 张志亮; 哈广浩

doi:10.3799/dqkx.2022.169

Volume 48 Issue 4

Apr. 2023

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Article Navigation > Earth Science > 2023 > 48(4): 1389-1404

Wu Dengyun, Ren Zhikun, Lü Honghua, Liu Jinrui, Lei Jinghao, Bao Guodong, Zhang Zhiliang, Ha Guanghao, 2023. Geomorphic Constraints on Listric Thrust Faulting: Implications for Active Deformation of Bayan Anticline in Youludusi Basin, East Tianshan, China. Earth Science, 48(4): 1389-1404. doi: 10.3799/dqkx.2022.169

Citation:

Wu Dengyun, Ren Zhikun, Lü Honghua, Liu Jinrui, Lei Jinghao, Bao Guodong, Zhang Zhiliang, Ha Guanghao, 2023. Geomorphic Constraints on Listric Thrust Faulting: Implications for Active Deformation of Bayan Anticline in Youludusi Basin, East Tianshan, China. Earth Science, 48(4): 1389-1404. doi: 10.3799/dqkx.2022.169

Citation:

Wu Dengyun, Ren Zhikun, Lü Honghua, Liu Jinrui, Lei Jinghao, Bao Guodong, Zhang Zhiliang, Ha Guanghao, 2023. Geomorphic Constraints on Listric Thrust Faulting: Implications for Active Deformation of Bayan Anticline in Youludusi Basin, East Tianshan, China. Earth Science, 48(4): 1389-1404. doi: 10.3799/dqkx.2022.169

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Geomorphic Constraints on Listric Thrust Faulting: Implications for Active Deformation of Bayan Anticline in Youludusi Basin, East Tianshan, China

doi: 10.3799/dqkx.2022.169

Wu Dengyun^{1, 2
,
,},
Ren Zhikun^{1, 2, 3
,
,},
Lü Honghua⁴,
Liu Jinrui^{1, 2},
Lei Jinghao^{1, 2},
Bao Guodong^{1, 2},
Zhang Zhiliang^{1, 2},
Ha Guanghao^{1, 2}

1.
Key Laboratory of Seismic and Volcanic Hazards, China Earthquake Administration, Beijing 100029, China
2.
Key Laboratory of Seismic and Volcanic Hazards, China Earthquake Administration, Beijing 100029, China
3.
Pamir National Intracontinental Subduction Scientific Observation and Research Station, Institute of Geology, China Earthquake Administration, Kashgar 844000, China
4.
School of Geographic Sciences, East China Normal University, Shanghai 200241, China

Received Date: 2022-03-09
Publish Date: 2023-04-25

Abstract

Abstract

Subsurface fault geometry and deformation rates can be estimated by combining the pattern of terrace deformation with kinematic model and geomorphic age. Quantifying the geometry, kinematics and deformation rate of the thrust-and-fold belt is the key to exploring tectonic deformation and strain distribution of the Tianshan intermontane basin. This is demonstrated by the Bayan anticline in Youlududsi basin in the eastern Chinese Tianshan. The Kaidu River, flowing through the central part of the Bayan anticline, has formed three terrace levels at tilted fold backlimbs. Based on the field geological investigation, warped and tilted terraces in the Bayan anticline are characterized by broad, continuous backlimbs and abrupt forelimbs and suggest folding through progressive limb rotation of listric thrust model. Combining with the kinematic model and geomorphic age, the slip rate and crustal shortening rate of the underlying fault in Bayan anticline is (0.35-0.06)-(0.35+0.16) mm/a and (0.23-0.04)-(0.23+0.10) mm/a, respectively. This shortening represents over 15%-20% of the total deformation in Youludusi basin and ~2% of the 8.5±0.5 mm/a total shortening rate measured from GPS velocity across the entire range in East Tianshan.Therefore, a significant fraction of the total Quaternary deformation is accommodated within the central part of the East Tianshan.
- listric thrust,
- terrace,
- Bayan anticline,
- Youludusi basin,
- Tianshan,
- structural geology

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References(48)

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Geomorphic Constraints on Listric Thrust Faulting: Implications for Active Deformation of Bayan Anticline in Youludusi Basin, East Tianshan, China

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