financially supported by the National Natural Science Foundation of China(Nos.41671005,41230743 and 41501068);the Distinguished Professor Programme of the Liaoning Province
We present geomorphological evidence for multiple glacial fluctuations during the Quaternary in the Taniantaweng Mountain, which is situated at the transition zone of the southeastern Qinghai-Tibet Plateau and the Yun...
Within Karakoram Himalaya, Hunza River Basin(study area) is unique for a number of reasons: 1) potential impacts of highly concentrated highpitched mountains and glacial ice; 2) the glaciated portions have higher mean...
supported by the China Geological Survey(grant Nos.DD20160048-04 and DD20179402-01 DD20179402-02);the National Natural Science Foundation of China(grant No.41702032)
Objective Northeast China is located in a cold region with high latitude. In the mid-low mountain areas, the existence of Quaternary glacier as well as its range and nature are always controversial. The glacial paleo...
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 area around Cangshan Mountain, located on the southeastern fringes of the Tibetan Plateau, is a key region in terms of revealing the processes involved in the uplifting of the Tibetan Plateau, plus its environment...
There are glacial remains of three different periods on the main peak of Snow Mountain in Taiwan province, including cirque lake, crosswall, polished surface, striation, moraine ete. These three different periods were...