吕梁山——华北克拉通中部中生代基底卷入褶皱系统

张北航; 张进; 曲军峰; 赵衡; 王艳楠; 李锦轶; 牛鹏飞; 赵硕; 郑荣国; 李岩峰; 云龙; 张义平; 惠洁

doi:10.3799/dqkx.2020.235

Volume 46 Issue 7

Jul. 2021

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Article Navigation > Earth Science > 2021 > 46(7): 2423-2448

Zhang Beihang, Zhang Jin, Qu Junfeng, Zhao Heng, Wang Yannan, Li Jinyi, Niu Pengfei, Zhao Shuo, Zheng Rongguo, Li Yanfeng, Yun Long, Zhang Yiping, Hui Jie, 2021. Lüliangshan: A Mesozoic Basement Involved Fold System in the Central North China Craton. Earth Science, 46(7): 2423-2448. doi: 10.3799/dqkx.2020.235

Citation:

Zhang Beihang, Zhang Jin, Qu Junfeng, Zhao Heng, Wang Yannan, Li Jinyi, Niu Pengfei, Zhao Shuo, Zheng Rongguo, Li Yanfeng, Yun Long, Zhang Yiping, Hui Jie, 2021. Lüliangshan: A Mesozoic Basement Involved Fold System in the Central North China Craton. Earth Science, 46(7): 2423-2448. doi: 10.3799/dqkx.2020.235

Citation:

Zhang Beihang, Zhang Jin, Qu Junfeng, Zhao Heng, Wang Yannan, Li Jinyi, Niu Pengfei, Zhao Shuo, Zheng Rongguo, Li Yanfeng, Yun Long, Zhang Yiping, Hui Jie, 2021. Lüliangshan: A Mesozoic Basement Involved Fold System in the Central North China Craton. Earth Science, 46(7): 2423-2448. doi: 10.3799/dqkx.2020.235

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Lüliangshan: A Mesozoic Basement Involved Fold System in the Central North China Craton

doi: 10.3799/dqkx.2020.235

1.
Key Laboratory of Deep-Earth Dynamics of Ministry of Natural Resources, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China
2.
School of Earth Science and Engineering, Hebei University of Engineering, Handan 056038, China
3.
National Earthquake Response Support Service, Beijing 100049, China
4.
Beijing Research Institute of Uranium Geology, Beijing 100029, China
5.
Chinese Academy of Geological Sciences, Beijing 100037, China
6.
College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing 100049, China

Received Date: 2020-08-07
Publish Date: 2021-07-15

Abstract

Abstract

The formation of the Lüliangshan located in the central North China Craton (NCC) is the result of the contraction event in the Late Jurassic-Early Cretaceous. In order to better understand the style, mechanism, background, and time of this deformation, a detailed field survey has been carried out in Lüliangshan area. The previous work of low temperature thermochronology has been collected. The results show that the Lüliangshan is a large basement involved fold system with typical monocline formed in Mesozoic in NCC. The existing foliations (i.e., gneissosity, schistosity, cleavage and joint) in the basement of the Precambrian orogenic belt in the central NCC reactivated to cause the folding of the overlying sedimentary layers during the later east-west shortening. The direction of shortening which resulted in the basement involved folds in the Lüliangshan is uniform across the entire mountain range, i.e., SE (122°)-NW (302°) compression. The mechanism, styles and distributions of monoclines in the Lüliangshan are similar to monoclines in the Laramide orogenic belt in the western North America. The folds including most monoclines in the Lüliangshan were formed in the Late Jurassic and caused by lower-angle subduction of the Paleo-Pacific Plate westwards, which also resulted in the intraplate contraction deformation of the NCC.
- Lü liangshan,
- Laramide,
- thick-shinned structure,
- North China Craton,
- Mesozoic,
- monocline,
- tectonics

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References(97)

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Lüliangshan: A Mesozoic Basement Involved Fold System in the Central North China Craton

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