土壤离子电导率方法在云南木利寻找隐伏锑矿的研究  

APPLICATION OF THE SOIL IONIC CONDUCTIVITY METHOD IN EXPLORATION OF BURIED ANTIMONY DEPOSITS IN MULI, YUNNAN PROVOINCE

作　　者：高锡根[1] 罗先熔[1] 单江涛[1] 吕明芬[1] 

机构地区：[1]桂林工学院隐伏矿床研究所,广西桂林541004

出　　处：《地质与资源》2009年第2期152-154,共3页Geology and Resources

摘　　要：土壤电导率找矿法是利用测定土壤溶液的导电性来发现隐伏矿体的一种找矿新方法.对已知锑矿土壤离子电导率的异常特征研究结果表明,利用该方法在云南木利地区寻找隐伏金矿是可行的.在木利锑矿矿区外围9km2范围内开展土壤的找矿预测研究,结果找到了3个有利的成矿靶区.The soil ionic conductivity is an efficient prospecting method to discover hidden ore bodies. Study on the abnormality of the soil ionic conductance of known antimony deposits shows that the method is feasible for prospecting buried antimony deposits in Muli, Yunnan Province. In an area of 9 square kilometers in the surroundings of the Muli antimony deposit, soil ionic conductivities are measured to predict hidden ores. As a result, three metallogenic targets are found.

关 键 词：土壤离子电导率 隐伏锑矿 找矿预测 云南木利 

分 类 号：P631.3[天文地球—地质矿产勘探]