Supported by the National Natural Science Foundation of China (Grant No. 40572126);China Earthquake Administration under project Integrated Investiga-tion of Seismogenic Structures for Intermediate-Strong Earthquakes in Jiashi-Bachu of Xinjiang Uygur Autonomous Region.
The Kalpin nappe structure is a strongest thrust and fold deformation belt in front of the Tianshan Mountains since the Cenozoic time. The tectonic deformation occurred in 5―6 striking Meso-zoic-Cenozoic fold zones, ...
This work was supported by the National Natural Science Foundation of China (Grant Nos.40325007 and 90102017) ;the Outstanding Overseas Chinese Scholars Fund of the ChineseAcademy of Sciences (Grant No.2003-01-07).
A typical sequence of fluvial terraces and aeolian deposits overlying these ter- races were multidisciplinary investigated. New evidences for uplift process of the northeastern Qinghai-Tibetan Plateau in the past 14 m...
This work was supported by the Foundation of the Tianshan Glaciology Station, the Chinese Academy of Sciences (Grant No. 9905);the National Natural Science Foundation of China (Grant Nos. 49971080 and 49731010);the Cold and Arid Regions Environment
The Shaerqiaoke Gravel, more than 400 m in thickness, on the north piedmont of the Tianshan Mountains, is located at the exit of the Urümqi River Valley and belongs to the Molasse construction of the Tianshan Mountai...