北京南观地区构造组合特征及成因机制

续海金; 王国庆; 舒坦; 刘德民

doi:10.3799/dqkx.2020.147

Volume 46 Issue 5

May 2021

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Xu Haijin, Wang Guoqing, Shu Tan, Liu Demin, 2021. Tectonic Pattern and Genetic Mechanism at Nanguan Area, West Hill of Beijing. Earth Science, 46(5): 1657-1676. doi: 10.3799/dqkx.2020.147

Citation:

Xu Haijin, Wang Guoqing, Shu Tan, Liu Demin, 2021. Tectonic Pattern and Genetic Mechanism at Nanguan Area, West Hill of Beijing. Earth Science, 46(5): 1657-1676. doi: 10.3799/dqkx.2020.147

Xu Haijin, Wang Guoqing, Shu Tan, Liu Demin, 2021. Tectonic Pattern and Genetic Mechanism at Nanguan Area, West Hill of Beijing. Earth Science, 46(5): 1657-1676. doi: 10.3799/dqkx.2020.147

Citation:

Xu Haijin, Wang Guoqing, Shu Tan, Liu Demin, 2021. Tectonic Pattern and Genetic Mechanism at Nanguan Area, West Hill of Beijing. Earth Science, 46(5): 1657-1676. doi: 10.3799/dqkx.2020.147

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Tectonic Pattern and Genetic Mechanism at Nanguan Area, West Hill of Beijing

doi: 10.3799/dqkx.2020.147

Xu Haijin^{1
,
,
,},
Wang Guoqing¹,
Shu Tan²,
Liu Demin¹

1.
School of Earth Sciences, China University of Geosciences, Wuhan 430074, China
2.
State Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China

Received Date: 2020-08-13
Publish Date: 2021-05-15

Abstract

Abstract

A series of tectonic association of the thrust nappe structure and the extensional tectonics are widely developed in the West Hill of Beijing, which are very important for understanding the tectonic evolution of the eastern part of North China craton (NCC). However, their deformed age, tectonic dynamic background and genetic mechanism are poorly understood. The Nanguan area in the West Hill of Beijing is an ideal place to decipher such a tectonic pattern. The detailed field structure observations show a tectonic association of the thrust nappe structure and the metamorphic core complex structure in the Nanguan area, generating a new type of tectonic pattern: the downward diapiric tectonics. It has the following characteristics: (1) wedge-shaped fold-fault structure with a normal fault along one side of the fold and a thrust fault along another side; (2) the fold (overturned syncline) is centered and both sides are older strata or basements, and (3) downward diapiric structure of the wedge-shaped body. Pudding-shaped lens of granitic and dioritic dykes were found in the thrust nappe. The granitic and dioritic lens give two weighted zircon U-Pb age of 141±2 Ma and 139±2 Ma, respectively. The previous studies suggest that a quartz monozite, which intruded into the thrust nappe, has zircon U-Pb age of 128-136 Ma. Thus, the deformation time of the thrust nappe is between ca. 140 and 130 Ma, which is a little earlier than or nearly coeval with the extensional tectonics represented by the metamorphic core complex structure. The orientation of the thrust nappe structure was generally W320°-335°N. The principal stress orientation of the extensional tectonics was also SE-NW trending. Thus, the tectonic pattern of compression-magmatism-extension in the West Hill of Beijing (and even in the eastern part of NCC) might be closely related to SE-NW-trending subduction of the Pacific plate. The tectonic pattern also might be an expression to the destroy or lithospheric thinning of the NCC.
- thrust nappe structure,
- metamorphic core complex structure,
- downward "diapiric" tectonics,
- tectonic regime,
- West Hill of Beijing,
- tectonics

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References(128)

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