焦作矿区电法探测导、含水构造的效果  

THE EFFECT OF D.C.METHOD USED TO DETECT WATER TRANSMITTING AND WATER BEARING STRUCTURE IN JIAOZUO MINING AREA

作　　者：张萍芳[1] 高建中[1] 徐少华 

机构地区：[1]焦作矿务局

出　　处：《煤田地质与勘探》1997年第5期40-43,共4页Coal Geology & Exploration

摘　　要：应用直流电法仪在井下进行了工作面巷道底板电测深和掘进头超前探测，查清了工作面底板含水层的富水性和掘进头前方的地质构造及含水情况。目前，大部分探测结果已得到生产实践的证实。Authors applied D.C.method instrument to electrical sounding of underworkings floor and the advance explo ration of driving face,and investigated the water abundance of the aquifer in underworkings floor,the geologic structures ahead of driving face and its water bearing conditions.At present,most of exploration results have been verified by the mining practices.

关 键 词：直流电法勘探 水文地质条件 矿井地质 含水构造 

分 类 号：TD166[矿业工程—矿山地质测量] P631.3[天文地球—地质矿产勘探]