Uplift processes for the Qinghai-Tibet Plateau: A comparative study of Yecheng section and Siwalik group

被引：1
|
作者：
Li, XZ [1 ]
Dong, GR
Chen, HH
Zheng, HB
Jin, HL
机构：
[1] Cold & Arid Regions Environm & Engn Res Inst, Lab Blown Sand Phys & Desert Environm, Lanzhou 730000, Peoples R China
[2] Tongji Univ, MOE Key Lab Marine Geol, Shanghai 200092, Peoples R China
[3] Chinese Acad Sci, Xian Open Lab Loess & Quaternary Geol, Xian 710054, Peoples R China
来源：
CHINESE SCIENCE BULLETIN | 2001年 / 46卷
关键词：
climate change; tectonic uplift; Qinghai-Tibet Plateau; Quaternary; Cenozoic;
D O I：
10.1007/BF03187248
中图分类号：
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号：
07 ; 0710 ; 09 ;
摘要：
Comparative studies of the Yecheng section at the northern piedmont of the Kunlun Mountain, and the Surai Khola section at the southern piedmont of the Himalayan Mountain, indicates that the Qinghai-Tibet Plateau is dominated by continuous uplift over the past 10 Ma. And the effective time scale for dividing the uplift stages would be 1 Ma. The uplift processes of the entire plateau can be divided mainly into three stages, i.e., a slow uplift stage (10.0-6.0 MaBP), a transitional uplift stage (6.0-2.5 MaBP) and a rapid uplift stage (since 2.5 MaBP). The plateau might have risen to 2000 m above sea level by 4.6 MaBP in response to uplift and to more than 3000 in by 2.5 MaBP.
引用
收藏
页码：108 / 113
页数：6
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