首页|Uplift of the Qinghai-Tibet Plateau: Lithospheric Structure and Structural Geomorphology of the Qinghai-Tibet Plateau

Uplift of the Qinghai-Tibet Plateau: Lithospheric Structure and Structural Geomorphology of the Qinghai-Tibet Plateau

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Through a review of the history of the study of the uplift of the Qinghai-Tibet Plateau and an analysis of various dynamic models of the uplift and on the basis of the strong inhomogeneity of the lithospheric structure of the Qinghai-Tibet Plateau and "tripartite" and "symmetric" structural geomorphologic pattern, the authors propose that the uplift of the Qinghai-Tibet Plateau is the result of integrated action of bidirectional differential subduction of the Indian block and the Tarim-Alxa block and the deep-seated thermal-uplift spreading beneath the interior of the Qinghai-Tibet Plateau.Subduction is an important mechanism of the uplift and thermal-uplift spreading is the direct cause.

geomorphologic patterndeep-seated thermal-upliftsubductionQinghai-Tibet Plateau

Cui Junwen、Li Pengwu、LI Li

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Institute of Geology, Chinese Acacemy of Geological Sciences, Beijing 100037, China

2001

大陆动力学(英文版)

大陆动力学(英文版)

ISSN：1006-7825
年,卷(期)：2001.6(2)
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