supported by the National Science Foundation of China(NSFC 41771005 and 41230743)。
Owing to the remoteness of the Longriba area and the lack of dating records,it is extremely challenging to reconstruct the chronology and extent of the paleoglaciers in this area.In this paper,we combined limited obse...
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...
supported by the National Natural Science Foundation of China(41101003,41230743,41328001,and 41371082);National Natural Science Awards of China(2009) to Yafeng Shi,Zhijiu Cui,Jijun Li,Benxing Zheng,and Shangzhe Zhou(Z104-2-05)
The onset of Quaternary glaciations is a critical event in the climate and tectonic history of the Tibetan Plateau.The Shishapangma Glaciation,defined based on the till deposit from the northern slopes of Mt.Shishapan...