摘要
古老滑坡往往规模大,变形持续缓慢。通过详实调查研究表明,池头滑坡具有显著的古老滑坡的系列特征。滑坡局部复活主要影响因素是后缘弃土石堆载加压、坡中耕作蓄水、前缘河流侵蚀和强降雨诱发。
Ancient landslides are often large-scaled with continuous but slow deformation. A study of the detailed investigations shows that the landslide has the features a typical ancient landslide. The main influencing factors for the partial resurrections are heap pressure at the trailing edge, farming impounding in the middle of the slope, river erosion at the front edge and heavy rainfall.
出处
《地质灾害与环境保护》
2014年第2期19-25,共7页
Journal of Geological Hazards and Environment Preservation
基金
福建省广义地质工作项目--福建省重大灾情地质灾害研究(20111201)
关键词
古滑坡
特征
复活
影响因素
ancient landslide
characteristics
resurrection
influencing factors
