The process and mechanism of the rise of the Qinghai-Tibet Plateau

被引：26

作者：

Li, TD

机构：

[1] Chinese Acad. of Geological Sciences, Fuchengmenwai, Beijing 100037

来源：

TECTONOPHYSICS | 1996年 / 260卷 / 1-3期

关键词：

D O I：

10.1016/0040-1951(96)00075-3

中图分类号：

P3 [地球物理学]; P59 [地球化学];

学科分类号：

0708 ; 070902 ;

摘要：

During the period from the Late Cretaceous to Eocene, the Qinghai-Tibet Plateau started a new stage of continental collision, crustal shortening and thickening and continuous rise. The rising process of the Plateau progressed through three stages. rise due to subduction collision, rise due to convergence compression and rise due to isostatic adjustment. The crustal thickening and shortening of the Plateau occurred through different modes of motion of the layers of the earth's crust. The model of the Plateau rise may be generalized as 'intracontinental convergence-crustal thickening-isostatic adjustment'.

引用

页码：45 / 53

页数：9