| 作成年度 | 2010 年度 |
|---|---|
| 論文名 | Relation between distance from earthquake source fault and scale of landslide triggered by recent two strong earthquakes in the Niigata Prefecture、 Japan |
| 論文名（和訳） | |
| 論文副題 | |
| 発表会 | INTERPRAEVENT 2010 |
| 誌名 | INTERPRAEVENT 2010 |
| 巻・号・回 | |
| 発表年月日 | 2010/04/01 |
| 所属研究室／機関名 | 著者名（英名） |
|---|---|
| Snow Avalanche and Landslide Research Center、 PWRI | Has Baator |
| Snow Avalanche and Landslide Research Center、 PWRI | Ishii Yasuo |
| Snow Avalanche and Landslide Research Center、 PWRI | Maruyama Kiyoteru |
| Nippon Koei、 Co.、 Ltd. | Suzuki Soki |
| National Institute for land and Infrastructure Management、 MLIT | Terada Hideki |
| 抄録 |
|---|
| Two strong earthquakes、 the Chuetsu earthquake (M6.8) in 2004 and the Chuetsu-offshore earthquake (M6.8) in 2007 struck the Niigata Prefecture、 eastern Japan、 caused a large number of landslides. To clarify the relationship between landslides scale and the distance from the earthquake source fault、 we interpreted and analysed the landslides induced by these two earthquakes. In the case of the Chuetsu earthquake、 362 landslides、 a total area of 5.15 km2 were interpreted in 1、003 km2 area. In the case of the Chuetsu-offshore earthquake、 18 landslides with total area of 0.06 km2 were recognized in 421 km2 area. The results showed that most of landslides occurred on the hanging-wall side of the source fault、 and landslides scale tends to decrease with increasing of distance from fault rupture. |
