羌塘-三江古生代-中生代沉积盆地演化

孔令耀; 姚华舟; 徐亚东; 骆满生; 罗亮; 吴旌

doi:10.3799/dqkx.2014.105

Volume 39 Issue 8

Aug. 2014

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Article Navigation > Earth Science > 2014 > 39(8): 1217-1229

Kong Lingyao, Yao Huazhou, Xu Yadong, Luo Mansheng, Luo Liang, Wu Jing, 2014. Evolution of Sedimentary Basins in Qiangtang-Sanjiang from Paleozoic to Mesozoic. Earth Science, 39(8): 1217-1229. doi: 10.3799/dqkx.2014.105

Citation:

Kong Lingyao, Yao Huazhou, Xu Yadong, Luo Mansheng, Luo Liang, Wu Jing, 2014. Evolution of Sedimentary Basins in Qiangtang-Sanjiang from Paleozoic to Mesozoic. Earth Science, 39(8): 1217-1229. doi: 10.3799/dqkx.2014.105

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Evolution of Sedimentary Basins in Qiangtang-Sanjiang from Paleozoic to Mesozoic

doi: 10.3799/dqkx.2014.105

Kong Lingyao^{1, 2
,},
Yao Huazhou^{2
,
,},
Xu Yadong^{3, 4},
Luo Mansheng³,
Luo Liang⁵,
Wu Jing⁴

1.
Institute of Geological Survey, China University of Geosciences, Wuhan 430074, China
2.
Wuhan Center of China Geological Survey, Wuhan 430205, China
3.
State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, China
4.
Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China
5.
Chengdu Center of China Geological Survey, Chengdu 610082, China

Received Date: 2014-06-05
Publish Date: 2014-08-01

Abstract

Abstract

The structure and evolution of Qiangtang-Sanjiang during Paleozoic-Mesozoic sedimentary basins were controlled by the Tethys. On the basis of the exploration of previous studies on lithostratigraphy, fossil assemblages, isotopic geochronology and tectonics of the study area, this paper classifies the sedimentary basins of Qiangtang-Sanjiang region, and analyzes the formation and evolution of each sedimentary basin. During the Early Paleozoic, Qiangtang-Sanjiang basins were mostly ocean environment; with the subduction of the Tethys Ocean to the northeastward and southeastward in Late Paleozoic, the active margin sedimentary basins developed in this area, forming Jinshajiang back arc-ocean, Lancangjiang back arc-ocean and Ganzi-Litang back arc-ocean and then the multiple island arc-basin systems of eastern Tethys system gradually formed. During the Mesozoic, with the subduction of the Tethys in Late Triassic in Qiangtang-Sanjiang, three arc-basins gradually closed, then large-scale arc-arc collision and arc-continent collision occurred in this area. This area eventually entered intracontinental evolution stage from the active margin sedimentary basins, Due to the close of Tethys in Cretaceous, the Indian plate and western China collided, inland basins developed in Qiangtang-Sanjiang.
- Qiangtang-Sanjiang,
- active continental margin,
- Tethys,
- sedimentology,
- tectonics,
- basin evolution

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References(103)

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Evolution of Sedimentary Basins in Qiangtang-Sanjiang from Paleozoic to Mesozoic

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