从青藏高原新生代构造隆升的时空差异性看青藏高原的扩展与高原形成过程

王国灿; 张克信; 曹凯; 王岸; 徐亚东; 孟艳宁

doi:10.3799/dqkx.2010.086.

Volume 35 Issue 5

Sep. 2010

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Article Navigation > Earth Science > 2010 > 35(5): 713-727

WANG Guo-can, ZHANG Ke-xin, CAO Kai, WANG An, XU Ya-dong, MENG Yan-ning, 2010. Expanding Processes of the Qinghai-Tibet Plateau during Cenozoic: An Insight from Spatio-Temporal Difference of Uplift. Earth Science, 35(5): 713-727. doi: 10.3799/dqkx.2010.086.

Citation:

WANG Guo-can, ZHANG Ke-xin, CAO Kai, WANG An, XU Ya-dong, MENG Yan-ning, 2010. Expanding Processes of the Qinghai-Tibet Plateau during Cenozoic: An Insight from Spatio-Temporal Difference of Uplift. Earth Science, 35(5): 713-727. doi: 10.3799/dqkx.2010.086.

Citation:

WANG Guo-can, ZHANG Ke-xin, CAO Kai, WANG An, XU Ya-dong, MENG Yan-ning, 2010. Expanding Processes of the Qinghai-Tibet Plateau during Cenozoic: An Insight from Spatio-Temporal Difference of Uplift. Earth Science, 35(5): 713-727. doi: 10.3799/dqkx.2010.086.

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Expanding Processes of the Qinghai-Tibet Plateau during Cenozoic: An Insight from Spatio-Temporal Difference of Uplift

doi: 10.3799/dqkx.2010.086.

WANG Guo-can^{1, 2
,},
ZHANG Ke-xin^{2, 3, 4},
CAO Kai²,
WANG An^{1, 2},
XU Ya-dong²,
MENG Yan-ning²

1.
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China
2.
Faulty of Earth Sciences, China University of Geosciences, Wuhan 430074, China
3.
Key Laboratory of Biogeology and Environmental Geology of Ministry of Education, China University of Geosciences, Wuhan 430074, China
4.
Geological Survey of China University of Geosciences, Wuhan 430074, China

Received Date: 2010-05-31
Available Online: 2021-11-10
Publish Date: 2010-09-01

Abstract

Abstract

In this paper we deduce the expanding and forming processes of the Qinghai-Tibet plateau by summarizing the spatio-temporal difference of uplift during Cenozoic. The uplift in the Paleocene-Eocene(65—35 Ma) mainly showed rock uplift driven by thrusting in different crust levels. The major denudation areas included the Tianshuihai, the Qilian Shan, Songpan-Ganzi-Bayan Har and Gangdise etc. There appeared alluvial-pluvial plain with low elevation in the Qiangtang-Hoh Xil-Qaidam and Xining-Linxia areas, and maritime space in the western Kunlun and Himalaya areas. In the Late Oligocene-Early Miocene (25—17 Ma), intensive thrusting induced increased crust thickness in the southern Tibet (including the Gangdese and the northern Himalayan belt). Then in about 17—12 Ma, crust isostatic compensation drove the southern Tibet to reach the current high elevation. Foreland basin developed in the Qiangtang-Hoh Xil area, and basin-range lelief emerged in the northern margin of the Qinghai-Tibet plateau during the late Oligocene-early Miocene. In the middle-late Miocene (13—7 Ma), centering in the southern Tibet (the Gangdise-northern Himalayan belt), the plateau grew and expanded northwardly. The basin in the Qiangtang-Hoh Xil area uplifted regionally and reached quite high altitude. In the northern margin of the Qinghai-Tibet plateau, a series of mountains ulteriorly popped up to the basin. The modern basin-range relief formed by and large but still kept lower average attitude. Since Pliocene, the plateau has been expanding northward rapidly. Rapid unitary surface uplift has been happening in the vast area of the Qiangtang-Hoh Xil-Songpan-Garzê-Bayan Har, forming the hinterland of the current plateau. In the northern edge of the plateau, the series of mountains also have been acutely uplifting and expanding forward adjacent basin, and average attitude has also been going up. In the Himalaya, the southern edge of the plateau, the relief contrast has been strengthening by thrusting and eroding. A series of high mountains finalize, with super-elevation of more than 7 000 m, such as the Qomolangma.
- Qinghai-Tibet plateau,
- tectonic uplift,
- surface uplift,
- plateau expanding

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References(131)

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Expanding Processes of the Qinghai-Tibet Plateau during Cenozoic: An Insight from Spatio-Temporal Difference of Uplift

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