摘要
2009年在安徽西梢地区铁矿普查过程中发现了地热异常,为了更加详细的了解地热异常信息判别断层含水性,2012年采用CSAMT法对异常区几条主断层进行了测量,结果表明CSAMT法在覆盖区寻找地热资源中有很好的反映。
Geothermal anomaly was found in the Xishao area of Anhui in 2009 in the course of iron exploration.In order to better understand the geothermal anomaly information and the water-bearing potential of fault,a survey was performed on several major faults in the anomalous area in 2012 using CSAMT,and the results indicated that CSAMT is effective in prospecting geothermal resources in overburden area.
出处
《安徽地质》
2017年第4期286-288,共3页
Geology of Anhui
关键词
CSAMT法
地热勘探
断裂构造
低阻带
张性断层
CSAMT
geothermal exploration
faulting structure
low-resistivity belt
tensile fault
