会议专题

Lessons We Learned from the Landslides Induced by the Wenchuan Earthquake and Its Application for the Future

Wenchuan earthquake induced numerous slope movements, of which distribution and direction were controlled by the earthquake faults and the geology. Landslides, which occurred on foliated rocks, such as phyllite, and some landslides of carbonate rocks were preceded by gravitational slope deformation. But many landslides of carbonate rocks occurred newly without topographic precursors. Landslides of valley fills were also induced by the earthquake without topographic precursors. These findings could be applied to the future landslide susceptibility evaluation.

Landslide Earthquake Fault Site prediction Geology

Masahiro Chigira Xiyong Wu Gonghui Wang Takashi Inokuchi

Disaster Prevention Research Institute, Kyoto University, Japan Southwest Jiaotong University, China Disaster Prevention Research Institute, Kyoto University, Japann National Research Institute for Earth Science and Disaster Prevention

国际会议

The First Anniversary of Wenchuan Earthquake(纪念汶川地震一周年国际学术会议)

成都

英文

64-71

2009-05-10(万方平台首次上网日期,不代表论文的发表时间)