Supported by the National Natural Science Foundation of China (40772175,40972175);the Scientific Research Fund of Southwest Jiaotong University(2008-A01);the Doctoral Student Innovation Fund of Southwest Jiaotong University;the National Natural Science Foundation of China-Yunan Joint Fund (U1033601)
Tangjiashan landslide is a typical high-speed landslide hosted on consequent bedding rock. The landslide was induced by Wenchuan earthquake at a medium-steep hill slope. The occurrence of Tangjiashan landslide was bas...
funding from the National Natural Science Foundation Project (Grant No. 40772175, 40972175);the Scientific research fund of Southwest Jiaotong University (Grant No.2008-A01);the Opening Fund of State Key Laboratory of Geohazard Prevention and Geoenvironment Protection (Chengdu University of Technology) (Grant No. DZKJ–08012);the National Natural Science Foundation Project-mutual fund of Yunnan Province (Grant No.U1033601)
Tangjiashan landslide is a typical high-speed consequent landslide of medium-steep dip angle. This landslide triggered by earthquake took place in about semi-minute. The relative sliding displacement is 900 meters, so...