上扬子地区中生代沉积盆地演化

韦一; 张宗言; 何卫红; 吴年文; 杨兵

doi:10.3799/dqkx.2014.095

Volume 39 Issue 8

Aug. 2014

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Wei Yi, Zhang Zongyan, He Weihong, Wu Nianwen, Yang Bing, 2014. Evolution of Sedimentary Basins in the Upper Yangtze during Mesozoic. Earth Science, 39(8): 1065-1078. doi: 10.3799/dqkx.2014.095

Citation:

Wei Yi, Zhang Zongyan, He Weihong, Wu Nianwen, Yang Bing, 2014. Evolution of Sedimentary Basins in the Upper Yangtze during Mesozoic. Earth Science, 39(8): 1065-1078. doi: 10.3799/dqkx.2014.095

Wei Yi, Zhang Zongyan, He Weihong, Wu Nianwen, Yang Bing, 2014. Evolution of Sedimentary Basins in the Upper Yangtze during Mesozoic. Earth Science, 39(8): 1065-1078. doi: 10.3799/dqkx.2014.095

Citation:

Wei Yi, Zhang Zongyan, He Weihong, Wu Nianwen, Yang Bing, 2014. Evolution of Sedimentary Basins in the Upper Yangtze during Mesozoic. Earth Science, 39(8): 1065-1078. doi: 10.3799/dqkx.2014.095

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Evolution of Sedimentary Basins in the Upper Yangtze during Mesozoic

doi: 10.3799/dqkx.2014.095

Wei Yi^{1, 2
,},
Zhang Zongyan^{2, 3},
He Weihong^{1, 2},
Wu Nianwen⁴,
Yang Bing^{1, 2}

1.
State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, China
2.
Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China
3.
Nanjing Institute of Geology and Mineral Resources, Nanjing 210016, China
4.
Wuhan Institute of Geology and Mineral Resources, Wuhan 430223, China

Received Date: 2014-03-16
Publish Date: 2014-08-01

Abstract

Abstract

The geotectonic environments are reconstructed and presented in this paper. Firstly, the Mesozoic sedimentary formation of the Upper Yangtze is studied in detail, then the basin features are analyzed based on the lithology of each unit (formation) and the space distribution framework of basins is established. Eventually, three stages of tectonic evolution of the Upper Yangtze are summarized by means of detailed analysis of chronostratigraphic and biostratigraphic correlations, paleogeography of biology, lithofacies and tectonics. The Upper Yangtze region rose continuously, water of which became shallow, and a series of clastic-carbonate epeiric sea and platform-interplatform basin sedimentary basin formed because of Indosinian orogeny during Early-Middle Triassic. When it came to Late Triassic to Early Jurassic, the Upper Yangtze collided with the Tethys domain block or arc-basin collisional zone in its west, the paleogeographic environments in the southwest and north of which turned to foreland basin and peripheral foreland basin, while the Xuefeng uplift turned orogeny. After middle Jurassic, with the subduction of paleo-Pacific plate to Asia plate, the south Upper Yangtze came into continental orogenic stage that mainly developed a series of downwarped basins to the east of Xuefeng Mountain and a large-scale depressional basin to the west.
- the Upper Yangtze,
- Mesozoic,
- sedimentology,
- basin-evolution,
- tectonics

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References(125)

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Evolution of Sedimentary Basins in the Upper Yangtze during Mesozoic

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