秦岭-大别新元古代-中生代沉积盆地演化

张思敏; 姜高磊; 柳坤峰; 王成刚

doi:10.3799/dqkx.2014.103

Volume 39 Issue 8

Aug. 2014

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Zhang Simin, Jiang Gaolei, Liu Kunfeng, Wang Chenggang, 2014. Evolution of Neoproterozoic-Mesozoic Sedimentary Basins in Qinling-Dabie Orogenic Belt. Earth Science, 39(8): 1185-1199. doi: 10.3799/dqkx.2014.103

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Zhang Simin, Jiang Gaolei, Liu Kunfeng, Wang Chenggang, 2014. Evolution of Neoproterozoic-Mesozoic Sedimentary Basins in Qinling-Dabie Orogenic Belt. Earth Science, 39(8): 1185-1199. doi: 10.3799/dqkx.2014.103

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Evolution of Neoproterozoic-Mesozoic Sedimentary Basins in Qinling-Dabie Orogenic Belt

doi: 10.3799/dqkx.2014.103

Zhang Simin^{1, 2
,},
Jiang Gaolei^{1, 2},
Liu Kunfeng^{2, 3},
Wang Chenggang⁴

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
4.
Wuhan Institute of Geology and Mineral Resources, Wuhan 430223, China

Received Date: 2014-04-12
Publish Date: 2014-08-01

Abstract

Abstract

As the eastern part of the Central Orogenic Belt, Qinling-Dabie Orogenic Belt has a complicated tectonic-sedimentary history. On the basis of a systematic research on the lithostratigraphy, fossil assemblages, isotopic geochronology and tectonics of 4 secondary and 13 three-level tectonic units, this paper divides the study area into 18 types of sedimentary basins, and discusses its tectonic-sedimentary evolution from Neoproterozoic to Mesozoic: (1) Neoproterozoic-Early Paleozoic: North Qinling was magmatic arc and forearc basin; South Qinling experienced intracontinental rift to interplatform basin-platform to continental-margin rift; Dabie-Sulu experienced intracontinental rift to interplatform basin-platform. (2) Late Paleozoic: North Qinling was marine-continental alternation epeiric sea; Mianlüe oceanic basin opened in the Devonian; South Qinling was backarc shelf and interplatform basin-platform at the same time. (3)Triassic: continental collision orogeny, stage of foreland basins. (4) Jurassic-Cretaceous: stage of fault basins and depressional basins.
- Qinling-Dabie,
- Neoproterozoic-Mesozoic,
- sedimentology,
- tectonics,
- basin evloution

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References(127)

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Evolution of Neoproterozoic-Mesozoic Sedimentary Basins in Qinling-Dabie Orogenic Belt

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