“V”型共轭走滑断裂：特征、形成机制及其对青藏高原东南缘晚新生代变形的启示

王锦涵; 石许华; 陈汉林; 杨蓉; 章凤奇; 程晓敢; 饶刚; 邓洪旦; 龚俊峰; 舒远海; 白卓娜

doi:10.3799/dqkx.2023.019

Volume 48 Issue 4

Apr. 2023

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Article Navigation > Earth Science > 2023 > 48(4): 1421-1440

Wang Jinhan, Shi Xuhua, Chen Hanlin, Yang Rong, Zhang Fengqi, Cheng Xiaogan, Rao Gang, Deng Hongdan, Gong Junfeng, Shu Yuanhai, Bai Zhuona, 2023. V-Shaped Conjugate Strike-Slip Faults: Characteristics, Formation Mechanisms and Implications for the Late Cenozoic Deformation in the Southeastern Tibetan Plateau. Earth Science, 48(4): 1421-1440. doi: 10.3799/dqkx.2023.019

Citation:

Wang Jinhan, Shi Xuhua, Chen Hanlin, Yang Rong, Zhang Fengqi, Cheng Xiaogan, Rao Gang, Deng Hongdan, Gong Junfeng, Shu Yuanhai, Bai Zhuona, 2023. V-Shaped Conjugate Strike-Slip Faults: Characteristics, Formation Mechanisms and Implications for the Late Cenozoic Deformation in the Southeastern Tibetan Plateau. Earth Science, 48(4): 1421-1440. doi: 10.3799/dqkx.2023.019

Citation:

Wang Jinhan, Shi Xuhua, Chen Hanlin, Yang Rong, Zhang Fengqi, Cheng Xiaogan, Rao Gang, Deng Hongdan, Gong Junfeng, Shu Yuanhai, Bai Zhuona, 2023. V-Shaped Conjugate Strike-Slip Faults: Characteristics, Formation Mechanisms and Implications for the Late Cenozoic Deformation in the Southeastern Tibetan Plateau. Earth Science, 48(4): 1421-1440. doi: 10.3799/dqkx.2023.019

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V-Shaped Conjugate Strike-Slip Faults: Characteristics, Formation Mechanisms and Implications for the Late Cenozoic Deformation in the Southeastern Tibetan Plateau

doi: 10.3799/dqkx.2023.019

Wang Jinhan^{1, 2
,
,},
Shi Xuhua^{1, 2
,
,
,},
Chen Hanlin^{1, 2},
Yang Rong^{1, 2},
Zhang Fengqi^{1, 2},
Cheng Xiaogan^{1, 2},
Rao Gang³,
Deng Hongdan^{1, 2},
Gong Junfeng^{1, 2},
Shu Yuanhai^{1, 2},
Bai Zhuona^{1, 2}

1.
Key Laboratory of Geoscience Big Data and Deep Resource of Zhejiang Province, School of Earth Sciences, Zhejiang University, Hangzhou 310058, China
2.
Structural Research Centre of Oil and Gas Bearing Basin of Ministry of Education, Hangzhou 310058, China
3.
School of Geoscience and Technology, Southwest Petroleum University, Chengdu 610500, China

Received Date: 2022-11-29
Publish Date: 2023-04-25

Abstract

Abstract

The V-shaped conjugate strike-slip fault system is defined as strike-slip faults with obtuse conjugate angles, whose opening side has an acute angle between the V-shaped faults, pointing to the direction of maximum extension. Previous studies on V-shaped conjugate strike-slip faults mostly focused on their development background and associated dynamic mechanisms. However, few literatures exist to comprehensively review the geometry and kinematics of V-shaped conjugate strike-slip faults. Here, we firstly summarize previous findings on the geometry, kinematic characteristics and formation mechanisms of existing V-shaped conjugate strike-slip faults, and then select the V-shaped conjugate strike-slip faults in the southeastern Tibetan Plateau for a case analysis. The characteristics of V-shaped conjugate strike-slip faults in the western United States, central and western Eurasian plate and central Tibet show a negative relation among conjugate angles and corresponding fault slip rates and fault lengths. The four formation mechanisms of the V-shaped conjugate strike-slip faults are 1) the fault planes experienced rotation after their formation, 2) the faults were reactivated along preexisting structurally weak zones, 3) the faults followed the paired general shear model and 4) the fault evolved according to the maximum-effective-moment criterion. Integrating analyses of geophysical data, elevation difference and geometric characteristics, we infer that the development of V-shaped conjugate strike-slip faults (Batang-Litang and Derong-Xiangcheng faults) in the Chuan-Dian block in the southeastern Tibetan Plateau, is consistent with gravitational spreading of the Tibetan lithosphere under the paired general shear model. This provides important insights for understanding the continuum crustal deformation in the southeastern Tibetan Plateau.
- V-shaped conjugate strike-slip faults,
- geometry,
- kinematics,
- formation mechanism,
- southeastern Tibetan Plateau,
- structural geology

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References(120)

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V-Shaped Conjugate Strike-Slip Faults: Characteristics, Formation Mechanisms and Implications for the Late Cenozoic Deformation in the Southeastern Tibetan Plateau

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