摘要
文章通过对四川锦屏山地区区域地质概况、河流阶地、第四纪断层及老断层新活动、地震活动的研究,认为该地区自更新世以来,新构造运动较为强烈,由此造成的地质灾害主要有滑坡、崩塌、泥石流等。
The results of research on the regional geology, geomorphology, river terraces, Quaternary faults and active old faults and earthquakes have revealed that the evidences of severe neotectonism that occurred from the Pleistocene onwards have been observed in the Jinping mountain area, resulting in the generation of the geologic disasters such as landslide, collapse and debris flows and earthquakes.
出处
《沉积与特提斯地质》
CAS
CSCD
2003年第1期99-104,共6页
Sedimentary Geology and Tethyan Geology
基金
中国地质调查局青藏高原南部空白区基础地质调查与研究(编号:121201310102)
青藏高原地质构造及其资源环境效应综合研究项目(编号:20011390069)
国土资源部区域地质调查新技术新方法集成示范研究项目(批准号2000201)
