摘要
通过高密度电阻率成像探测法,在王家坡滑坡体勘察中建立了滑坡体地质特征—电性特征解释模型,查明了滑坡体的空间特征,并根据实际情况,推断了新的滑坡体位置,认为现存滑坡体中部及前缘存在潜在的次级滑体,后期可能会出现滑坡前缘前移。
By means of high density resistivity imaging method,an interpretation model of geological and electrical characteristics of landslide was established and the spatial characteristics of landslide were identified during investigation in Wangjiapo landslide.According to the actual situation,a new landslide position is deduced.It is considered that there are potential secondary landslides in the middle and front of the existing landslide body,and the front of the landslide may move forward in the later period.
作者
庞日轩
刘铁铭
李西周
田靖
杨帅
赵峰
Pang Ri-xuan;Liu Tie-ming;Li Xi-zhou;Tian-jing;Yang Shuai;Zhao Feng(Shaanxi Geophysical and Geochemical Exploration Team of Shaanxi Corporationof Geology and Mineral Development,Xi’an 710043;Xi’an Geo-environment Monitoring Station,Xi’an 710007)
出处
《陕西地质》
2019年第1期79-85,共7页
Geology of Shaanxi
关键词
高密度电法
黄土滑坡
应用
high density electrical method
loess landslide
application
