Rising process of the Qinghai-Xizang (Tibet) Plateau and its mechanism

被引:0
|
作者
钟大赉
丁林
机构
[1] Institute of Geology
[2] Chinese Academy of Sciences
[3] Laboratory of Lithosphcre Tectonic Evolution
[4] Beijing 100029
[5] China
基金
中国国家自然科学基金;
关键词
fission-track dating; rising process; mechanisms of uplift; Qinghai-Xizang Plateau;
D O I
暂无
中图分类号
P542.2 [];
学科分类号
070904 ;
摘要
The rising of the Qinghai-Xizang Plateau has character of multistage (45-38 Ma, 25-17 Ma, 13-8 Ma, 3 Ma-present), inhomogeneity and hetero-speed. The whole uprising of the plateau and local rapid rising in its periphery since Late Pliocene is a synthetical result of at least two or more mechanisms.
引用
收藏
页码:369 / 379
页数:11
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