supported by the National Natural Science Foundation of China(Grant Nos.41971009&41503054);the Strategic Priority Research Program of Chinese Academy of Sciences(Grant No.XDA2000300)。
The Hengduan Mountains is in the transitional zone between the Qinghai-Tibet Plateau(QTP)and the YunnanGuizhou Plateau in China,and a key area for elucidating the Quaternary environmental changes in Asia.The paleo-Dao...
supported by National Natural Science Foundation of China (Grant Nos.40801033 and 41130529);DFG,German Research Foundation (Grant No.BR1895/21-1)
Fluctuation history of Midui glacier in the southeastern Tibet since the Little Ice Age(LIA) was reconstructed by the dating of lateral and terminal moraines using tree rings.Four conversions of glacier advance/stabil...
supported by National Natural Science Foundation of China(Grant No.40771049);Knowledge Innovation Project of Chinese Academy of Sciences(Grant No.KZCX2-YW-GJ04);the Program of Ministry of Science and Technology of China(Grant No. 2006FY110200)
Kongur Mountain is the largest center of modern glaciation on the Pamir Plateau.During the glacial-interglacial cycles of the Quaternary,Kongur Mountain was extensively and repeatedly glaciated,and the glacial landfor...
The research was supported in part by the National Natural Science Foundation of China (Grant No.79972077).
This research focused on the Aksu area in the central part of the southern Tianshan. Along the 60 km wide Aksu fold-and-thrust belt, active thrusts reach the surface and offset the youngest sediments. Our research was...
Project supported by Xi'an Laboratory of Loess and Quaternary Geology and by funds of National Planning Committee of China.
Correlation of the loess-paleosol sequence on Loess Plateau and the tectonodimatic cycle it reflects with the moraine-paleosol sequence on Qingbai-Xizang Plateau and the uplift process it reflects, indicates that both...