东吴运动性质的厘定及其时空演变规律

何斌; 徐义刚; 王雅玫; 肖龙

Volume 30 Issue 1

Jan. 2005

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HE Bin, XU Yi-gang, WANG Ya-mei, XIAO Long, 2005. Nature of the Dongwu Movement and Its Temporal and Spatial Evolution. Earth Science, 30(1): 89-96.

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HE Bin, XU Yi-gang, WANG Ya-mei, XIAO Long, 2005. Nature of the Dongwu Movement and Its Temporal and Spatial Evolution. Earth Science, 30(1): 89-96.

HE Bin, XU Yi-gang, WANG Ya-mei, XIAO Long, 2005. Nature of the Dongwu Movement and Its Temporal and Spatial Evolution. Earth Science, 30(1): 89-96.

Citation:

HE Bin, XU Yi-gang, WANG Ya-mei, XIAO Long, 2005. Nature of the Dongwu Movement and Its Temporal and Spatial Evolution. Earth Science, 30(1): 89-96.

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Nature of the Dongwu Movement and Its Temporal and Spatial Evolution

HE Bin^{1, 2
,},
XU Yi-gang¹,
WANG Ya-mei²,
XIAO Long²

1.
Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China
2.
Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China

Received Date: 2004-04-28
Publish Date: 2005-01-25

Abstract

Abstract

Dongwu movement is an important geological event of the Permian in South China, however, there are still lots of disputes and controversy on the timing, dimension and nature of the Dongwu movement. This paper discusses the nature, geodynamics and evolution of the Dongwu movement. It is based on biostratigraphic correlation of the Maokou Formation and the study of an unconformity and volcanism in the Upper Yangtze block, combined with an analysis of the stratigraphy, sedimentation, lithofacies and paleogeography of the Permian in South China. This research suggests that there is a genetic relationship between the rising of the Emeishan mantle-plume, the eruption of the Emeishan basalts, and the Dongwu movement. That is, the Dongwu movement is a rapid differential crustal uplift caused by the rising of the Emeishan mantle-plume. It is stronger in the west than in the east, and it began earlier in the west. This research also shows that the Dongwu movement did not extend as far as the lower Yangtze and south Huanan block, and that the sedimentation in these areas during the Permian was controlled by the Huanan block.
- Dongwu movement,
- Yangtze platform,
- Permian,
- Emeishan basalts,
- mantle plume,
- crustal uplift

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References(44)

References

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