funded by National Natural Science Foundation of China(No.40802052);the National Basic Research Program of China(2004CB418401)
Quantitative analysis of the kinematics of the active faults distributed around the QinghaiTibetan Plateau is critical to understand current tectonic processes of the plateau. Chronological analysis, based on the comp...
supported by Special Foundation of China Earthquake Administration(Grant No.200808016);National Basic Research Program of China(Grant No.2004CB418401)
Trenching is a primary technique on paleoseismology to reveal evidence of surface deformation produced by large earthquakes.A good trenching site requires completeness of geologic recording on paleoseismic events and ...
supported by National Basic Research Program of China (Grant No. 2004CB418401)
This study reconstructs the long-term evolution of river terraces over large spatial scales along the Anning River, western Sichuan, and identifies external factors controlling terrace formation. Pollen record analysi...
supported by the National Basic Research Program of China(Grant No.2004CB418401);National Science Foundation of China(grant No.40841007)
On May 12th, 2008, the Mw7.9 Wenchuan earthquake ruptured the Beichuan, Pengguan and Xiaoyudong faults simultaneously along the middle segment of the Longmenshan thrust belt at the eastern margin of the Tibetan platea...