北京西山白垩纪-古近纪多期次构造叠加作用：以周口店黄院奥陶系变形为例

刘先益; 梁晓; 干微; 王根厚; 徐德兵; 魏玉帅; 张宏远; 李加斌; 黄祖根

doi:10.3799/dqkx.2020.269

Volume 46 Issue 4

Apr. 2021

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Article Navigation > Earth Science > 2021 > 46(4): 1467-1480

Liu Xianyi, Liang Xiao, Gan Wei, Wang Genhou, Xu Debing, Wei Yushuai, Zhang Hongyuan, Li Jiabin, Huang Zugen, 2021. Multiple-Stage Structural Superimposition of Cretaceous-Paloegene Deformation in West Hill of Beijing: An Example from the Ordovician Carbonate Rocks in Huangyuan, Zhoukoudian. Earth Science, 46(4): 1467-1480. doi: 10.3799/dqkx.2020.269

Citation:

Liu Xianyi, Liang Xiao, Gan Wei, Wang Genhou, Xu Debing, Wei Yushuai, Zhang Hongyuan, Li Jiabin, Huang Zugen, 2021. Multiple-Stage Structural Superimposition of Cretaceous-Paloegene Deformation in West Hill of Beijing: An Example from the Ordovician Carbonate Rocks in Huangyuan, Zhoukoudian. Earth Science, 46(4): 1467-1480. doi: 10.3799/dqkx.2020.269

Citation:

Liu Xianyi, Liang Xiao, Gan Wei, Wang Genhou, Xu Debing, Wei Yushuai, Zhang Hongyuan, Li Jiabin, Huang Zugen, 2021. Multiple-Stage Structural Superimposition of Cretaceous-Paloegene Deformation in West Hill of Beijing: An Example from the Ordovician Carbonate Rocks in Huangyuan, Zhoukoudian. Earth Science, 46(4): 1467-1480. doi: 10.3799/dqkx.2020.269

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Multiple-Stage Structural Superimposition of Cretaceous-Paloegene Deformation in West Hill of Beijing: An Example from the Ordovician Carbonate Rocks in Huangyuan, Zhoukoudian

doi: 10.3799/dqkx.2020.269

1.
School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China
2.
Department of Earth Science, University College London, London WC1E 6BT, The United Kingdom

Received Date: 2020-06-19
Publish Date: 2021-04-15

Abstract

Abstract

The West Hill of Beijing experienced multiple stages of deformation since Mesozoic,and is considered as an important window to decipher the tectonic evolution of the North China block. Structural analyses and the EBSD data show that the Ordovician carbonate rocks in Huangyuan of Zhoukoudian is characterized by four stages of deformation,among which the D₂ NE-SW-striking compressional structures shaped the main structural style. The D₁ is represented by top-to-the-SEE (110°-120°) shearing bands and the penetrative stretching lineation L₁,and the pervasive foliation S₁ has replaced the sedimentary bedding S₀. From north to south,the D₂ deformation can be subdivided into two subzones including buckle fold and ductile shear zone,showing a consistent kinematics of top-to-the-SE thrusting as indicated by the fold vergence and shearing bands,respectively. The D₃ is featured by the NWW-directed normal slipping superimposed on the foliation S₂,and the D₄ displays nearly N-S-trending high-angle normal faults. According to the youngest zircon U-Pb age peak (~116 Ma) of a diorite intrusion,it infers that the D₁ happened in the late Early Cretaceous,and the D₂ occurred in the Late Cretaceous,i.e.,the Late Yanshanian stage,probably as a response to the continental-continental collision after the closure of the Mongol-Okhotsk Ocean.
- West Hill of Beijing,
- multiple-stage deformation,
- structure,
- Ordovician,
- Cretaceous,
- structural geology

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References(53)

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Multiple-Stage Structural Superimposition of Cretaceous-Paloegene Deformation in West Hill of Beijing: An Example from the Ordovician Carbonate Rocks in Huangyuan, Zhoukoudian

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