Late Paleogene sinistral strike-slip system along east Qinling and in southern North China: Implications for interaction between collision-related block trans-rotation and subduction-related back-arc extension in East China
We present in this paper a compilation of Paleogene rift and strike-slip structures in east Qinling and southern North China based on a synthesis of published stratigraphic, structural and thermochronological data, which aids in delineating a broad (>500-km-wide), kinematically interlinked, Eocen...
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| Published in | Tectonophysics Vol. 769; p. 228181 |
|---|---|
| Main Authors | , , |
| Format | Journal Article |
| Language | English |
| Published |
Amsterdam
Elsevier B.V
20.10.2019
Elsevier BV |
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| Abstract | We present in this paper a compilation of Paleogene rift and strike-slip structures in east Qinling and southern North China based on a synthesis of published stratigraphic, structural and thermochronological data, which aids in delineating a broad (>500-km-wide), kinematically interlinked, Eocene-Oligocene transtensional system. This transtensional system was bifurcated from two discrete strike-slip fault zones in NE Tibetan Plateau. The overall fault patterns indicate a clockwise rotation of South China relative to North China during the Cenozoic, possibly driven by dextral shearing along the eastern Tibetan margin. This collision-related trans-rotation of South China occurred coevally with late Paleogene intracontinental rifting and volcanism in East China in a subduction-related back-arc extensional setting. These two tectonic processes interacted with each other, giving birth to Cenozoic rift systems and contrasting morpho-structural features in East Asia.
•Delineation of Paleogene rifts in East China and major rifting phases and tectonic inversion events.•Depicting late Paleogene sinistral strike-slip system along east Qinling.•Interaction between collision-related transrotation and subduction-related back-arc extension in East China. |
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| AbstractList | We present in this paper a compilation of Paleogene rift and strike-slip structures in east Qinling and southern North China based on a synthesis of published stratigraphic, structural and thermochronological data, which aids in delineating a broad (>500-km-wide), kinematically interlinked, Eocene-Oligocene transtensional system. This transtensional system was bifurcated from two discrete strike-slip fault zones in NE Tibetan Plateau. The overall fault patterns indicate a clockwise rotation of South China relative to North China during the Cenozoic, possibly driven by dextral shearing along the eastern Tibetan margin. This collision-related trans-rotation of South China occurred coevally with late Paleogene intracontinental rifting and volcanism in East China in a subduction-related back-arc extensional setting. These two tectonic processes interacted with each other, giving birth to Cenozoic rift systems and contrasting morpho-structural features in East Asia.
•Delineation of Paleogene rifts in East China and major rifting phases and tectonic inversion events.•Depicting late Paleogene sinistral strike-slip system along east Qinling.•Interaction between collision-related transrotation and subduction-related back-arc extension in East China. We present in this paper a compilation of Paleogene rift and strike-slip structures in east Qinling and southern North China based on a synthesis of published stratigraphic, structural and thermochronological data, which aids in delineating a broad (>500-km-wide), kinematically interlinked, Eocene-Oligocene transtensional system. This transtensional system was bifurcated from two discrete strike-slip fault zones in NE Tibetan Plateau. The overall fault patterns indicate a clockwise rotation of South China relative to North China during the Cenozoic, possibly driven by dextral shearing along the eastern Tibetan margin. This collision-related trans-rotation of South China occurred coevally with late Paleogene intracontinental rifting and volcanism in East China in a subduction-related back-arc extensional setting. These two tectonic processes interacted with each other, giving birth to Cenozoic rift systems and contrasting morpho-structural features in East Asia. |
| ArticleNumber | 228181 |
| Author | Zhang, Yueqiao Dong, Shuwen Li, Jianhua |
| Author_xml | – sequence: 1 givenname: Yueqiao surname: Zhang fullname: Zhang, Yueqiao email: zhangyq@nju.edu.cn organization: School of Earth Sciences and Engineering, Nanjing University, Jiangsu Province, Nanjing 210023, China – sequence: 2 givenname: Shuwen surname: Dong fullname: Dong, Shuwen organization: Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 10081, China – sequence: 3 givenname: Jianhua surname: Li fullname: Li, Jianhua organization: Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 10081, China |
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| Keywords | Collision-related trans-rotation East Qinling Eocene-Oligocene sinistral strike-slip system Plate tectonic process interaction Subduction-related back-arc extension |
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| Snippet | We present in this paper a compilation of Paleogene rift and strike-slip structures in east Qinling and southern North China based on a synthesis of published... |
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| SubjectTerms | Bifurcations Cenozoic Collision-related trans-rotation East Qinling Eocene Eocene-Oligocene sinistral strike-slip system Fault zones Geological faults Magma Oligocene Paleogene Plate tectonic process interaction Rift zones Rifting Rotation Shearing Slip Stratigraphy Subduction Subduction (geology) Subduction-related back-arc extension Tectonic processes Tectonics Volcanic activity Volcanism |
| Title | Late Paleogene sinistral strike-slip system along east Qinling and in southern North China: Implications for interaction between collision-related block trans-rotation and subduction-related back-arc extension in East China |
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