| Based on analysis of earthquake-induced landslide distributions with the peak ground acceleration and seismic intensity (in JMA scale), distance from the source fault, the results revealed that: 1) Most of the landslides occurred in the area where the PGA is larger than 500 gal, and the maximum seismic intensity is larger than 5 plus ; 2) The landslides occurred in a short distance from the source fault (the shortest distance from the surface projection of top tip of the fault; 3) More than 80% of landslides occurred on the hanging wall, and the size of landslide is larger than that occurred on the footwall of the source fault; 4) The number and size of landslide tends to deceases with the distance from the source fault. |
