华北陆块新元古代-中生代沉积盆地划分及其构造演化

郝奕玮; 骆满生; 徐增连; 邹亚锐; 唐婷婷

doi:10.3799/dqkx.2014.106

Volume 39 Issue 8

Aug. 2014

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Article Navigation > Earth Science > 2014 > 39(8): 1230-1242

Hao Yiwei, Luo Mansheng, Xu Zenglian, Zou Yarui, Tang Tingting, 2014. Division of Sedimentary Basins and Its Tectonic Evolution in North China from Newproterozoic to Mesozoic. Earth Science, 39(8): 1230-1242. doi: 10.3799/dqkx.2014.106

Citation:

Hao Yiwei, Luo Mansheng, Xu Zenglian, Zou Yarui, Tang Tingting, 2014. Division of Sedimentary Basins and Its Tectonic Evolution in North China from Newproterozoic to Mesozoic. Earth Science, 39(8): 1230-1242. doi: 10.3799/dqkx.2014.106

Citation:

Hao Yiwei, Luo Mansheng, Xu Zenglian, Zou Yarui, Tang Tingting, 2014. Division of Sedimentary Basins and Its Tectonic Evolution in North China from Newproterozoic to Mesozoic. Earth Science, 39(8): 1230-1242. doi: 10.3799/dqkx.2014.106

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Division of Sedimentary Basins and Its Tectonic Evolution in North China from Newproterozoic to Mesozoic

doi: 10.3799/dqkx.2014.106

Hao Yiwei^{1, 2
,},
Luo Mansheng^{2
,
,},
Xu Zenglian^{1, 2},
Zou Yarui^{1, 3},
Tang Tingting^{1, 3}

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

Received Date: 2013-05-28
Publish Date: 2014-08-01

Abstract

Abstract

On the basis of divisions of tectonic-stratum of the North China block (NCB) area, this article discusses the type of sedimentary basins formation region, filling sequence and temporal evolution of different tectonic-stratum zones for each construction phase according to five tectonic stages as Mesoproterozoic-Neoproterozoic, Paleozoic, Late Paleozoic, Triassic-Early Jurassic, Middle Jurassic-Cretaceous. Meso-Neoproterozoic is the stage of development of periphery rifting. Cambrian-Early, Middle Ordovician, North China plate synchronized global settlement and received extensive transgression, forming widespread carbonate platform of almost all north China. Late Ordovician-Devonian, NCB overall uplift and erosion, sedimentation is missing. Carboniferous-Permian, North China block subsided again and suffered transgression, forming a broad epicontinental sea paralic deposition. To Late Permian, NCB entered the stage of continental basin development. Mesozoic, continental tectonic activities were active, forming fault basins, sag basins and pull-apart basins broadly.
- sedimentology,
- tectonics,
- Neoproterozoic-Mesozoic,
- North China,

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References(83)

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Division of Sedimentary Basins and Its Tectonic Evolution in North China from Newproterozoic to Mesozoic

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