班公湖-双湖-怒江-昌宁-孟连新元古代-中生代沉积盆地演化

罗亮; 安显银; 吴年文; 王成刚; 战虹宇

doi:10.3799/dqkx.2014.102

Volume 39 Issue 8

Aug. 2014

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Article Navigation > Earth Science > 2014 > 39(8): 1169-1184

Luo Liang, An Xianyin, Wu Nianwen, Wang Chenggang, Zhan Hongyu, 2014. Evolution of Neoproterozoic-Mesozoic Sedimentary Basins in Bangonghu-Shuanghu-Nujiang-Changning-Menglian Suture Zone. Earth Science, 39(8): 1169-1184. doi: 10.3799/dqkx.2014.102

Citation:

Luo Liang, An Xianyin, Wu Nianwen, Wang Chenggang, Zhan Hongyu, 2014. Evolution of Neoproterozoic-Mesozoic Sedimentary Basins in Bangonghu-Shuanghu-Nujiang-Changning-Menglian Suture Zone. Earth Science, 39(8): 1169-1184. doi: 10.3799/dqkx.2014.102

Citation:

Luo Liang, An Xianyin, Wu Nianwen, Wang Chenggang, Zhan Hongyu, 2014. Evolution of Neoproterozoic-Mesozoic Sedimentary Basins in Bangonghu-Shuanghu-Nujiang-Changning-Menglian Suture Zone. Earth Science, 39(8): 1169-1184. doi: 10.3799/dqkx.2014.102

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Evolution of Neoproterozoic-Mesozoic Sedimentary Basins in Bangonghu-Shuanghu-Nujiang-Changning-Menglian Suture Zone

doi: 10.3799/dqkx.2014.102

Luo Liang^{1, 2
,},
An Xianyin^{1, 2},
Wu Nianwen^{2, 3},
Wang Chenggang^{2, 3},
Zhan Hongyu⁴

1.
Chengdu Institute of Geology and Mineral Resources, Chengdu 610081, China
2.
Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China
3.
Wuhan Institute of Geology and Mineral Resources, Wuhan 430223, China
4.
Institute of Geophysics & Geomatics, China University of Geosciences, Wuhan 430074, China

Received Date: 2013-04-25
Publish Date: 2014-08-01

Abstract

Abstract

In the light of the stratigraphic framework, the authors collected and summarized evidences of the rock formations and their ages in the sedimentary basins of the Bangonghu-Shuanghu-Nujiang-Changning-Menglian suture zone. With the guidance of the plate tectonic theory and continental dynamics, the basin types are also classified in the study area to explore the temporal and spatial evolution of the basins and to better the understanding of the opening, extension and closing of the Paleo-Tethys oceans. Four evolutional stages of the Pre-Cenozoic Paleo-Tethys oceans corresponding to the basinal evolution in the study area are distinguished. It is found that Ordovician ophiolitic mélange of MORB characteristics occurred in both the Longmu-Shuanghu and the Changning-Menglian oceanic basin, two of which prove to have experienced arc-continent collision during the end Permian-Early Triassic transition, suggesting a united remnant oceanic basin of the Paleo-Tethys. The remnant Paleo-Tethys represented by the Bangonghu-Nujiang oceanic basin, on the other hand, opened in the Early Carboniferous and evolved to a closure in the Early Cretaceous, marking the final disappearance of the Paleo-Tethys.
- ophilitic mélange,
- Paleo-Tethys,
- stratigraphic framework,
- sedimentology,
- tectonics,
- basin evolution

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References(141)

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Evolution of Neoproterozoic-Mesozoic Sedimentary Basins in Bangonghu-Shuanghu-Nujiang-Changning-Menglian Suture Zone

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