北京房山地区太平山褶皱的变形特征和形成时代:华北克拉通早白垩世挤压构造的意义

舒坦; 续海金; 章军锋; 刘强

doi:10.3799/dqkx.2018.119

Volume 44 Issue 5

May 2019

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Article Navigation > Earth Science > 2019 > 44(5): 1734-1748

Shu Tan, Xu Haijin, Zhang Junfeng, Liu Qiang, 2019. Deformation Characteristics and Time of Taipingshan Folds in Fangshan Area, Beijing: Implications for Early Cretaceous Compressional Tectonics of North China Craton. Earth Science, 44(5): 1734-1748. doi: 10.3799/dqkx.2018.119

Citation:

Shu Tan, Xu Haijin, Zhang Junfeng, Liu Qiang, 2019. Deformation Characteristics and Time of Taipingshan Folds in Fangshan Area, Beijing: Implications for Early Cretaceous Compressional Tectonics of North China Craton. Earth Science, 44(5): 1734-1748. doi: 10.3799/dqkx.2018.119

Citation:

Shu Tan, Xu Haijin, Zhang Junfeng, Liu Qiang, 2019. Deformation Characteristics and Time of Taipingshan Folds in Fangshan Area, Beijing: Implications for Early Cretaceous Compressional Tectonics of North China Craton. Earth Science, 44(5): 1734-1748. doi: 10.3799/dqkx.2018.119

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Deformation Characteristics and Time of Taipingshan Folds in Fangshan Area, Beijing: Implications for Early Cretaceous Compressional Tectonics of North China Craton

doi: 10.3799/dqkx.2018.119

School of Earth Sciences, China University of Geosciences, Wuhan 430074, China

Received Date: 2019-01-06
Publish Date: 2019-05-15

Abstract

Abstract

The folds with near E-W-trending fold axis are widely developed in the Western Hills of Beijing, which are very important for understanding the tectonic evolution of the eastern part of North China craton (NCC). However, their deformation age and tectonic dynamic background are poorly understood. Taipingshan folds in the Fangshan area, Beijing, are typical folds with near E-W axial orientation. The detailed field structure observation and tectonic geochronology were carried out to determine the spatial distribution characteristics and tectonic style of Taipingshan folds and their deformation age. The detailed field structure observation and systematic β-diagrams study show that the Taipingshan folds consist of an upright capsized anticline and an inclined capsized syncline. A deformed lamprophyre sheet which is earlier than the folds structure gives a weighted zircon U-Pb age of 147.2±2.4 Ma, and the later porphyrite dyke that cuts strata of the folds gives a weighted zircon U-Pb age of 129.0±3.2 Ma, suggesting that the deformation time of the Taipingshan folds is between ca. 147 and 129 Ma, belonging to phase B of "Yanshanian movement". In addition, the extensional structure with NW-SE extensional direction is also developed in the Western Hills of Beijing. Fangshan dome (about 136 Ma), which is a typical product of the extensional tectonic, intruded into and cut the Taipingshan folds, further limiting the deformation age of the Taipingshan folds ranges from ca. 147 to 136 Ma. Thus, the folds with E-W-trending fold axis in the studied area are products of nearly N-S compressional tectonics in Early Cretaceous. The tectonic regime transformation from N-S compressional to NW-SE extensional tectonics provides a key understanding on tectonic dynamics of the eastern part of NCC in Late Mesozoic.
- tectonic deformation,
- deformation time,
- tectonic regime,
- Western Hills of Beijing,
- North China craton,
- tectonics

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References(112)

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Deformation Characteristics and Time of Taipingshan Folds in Fangshan Area, Beijing: Implications for Early Cretaceous Compressional Tectonics of North China Craton

doi: 10.3799/dqkx.2018.119

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