摘要
对临沧市南撒至班考二级公路山体地质灾害勘察中,地质雷达取得了较好的地质效果,确定地下岩溶发育区的空间展布规律、岩溶破碎带的形态及延伸,为进一步认识山体地质灾害及其勘察治理提供了地球物理依据。
In the exploration of mountain geological disaster of rank 2 highway from Nansa to Bankao of Lincang,the geological result of geological radar is good,which has determined the distribution rule of underground karst development area,the form and extension of karst fracture zone.It can provide the geophysical basis in the future investigation of mountain geological disaster and the exploration-control of disaster.
出处
《云南地质》
2012年第3期417-419,共3页
Yunnan Geology
关键词
地质雷达探测
喀斯特洞穴
岩溶破碎带
介电常数差异
云南省临沧市
Geological Radar Exploration
Karst Cave
Karst Fracture Zone
Difference of Dielectric Constant
Lincang,Yunnan
