广西平桂地区隐伏钨锡矿床土壤离子电导率异常特征  

AN IONIC CONDUCTIVITY ANOMALY CHARACTER IN SOILCOVER OF THE TIN-TUNGSTEN ORE DEPOSITS IN PINGGUI AREA,GUANGXI

作　　者：罗先熔[1] 

机构地区：[1]桂林冶金地质学院

出　　处：《桂林冶金地质学院学报》1989年第1期99-104,共6页

摘　　要：平桂地区不同隐伏矿床上方,土壤离子电导率异常的特征不同。根据电导率异常的特征及其差异,能够进行隐伏矿床预测,区分隐伏矿床类型。本文以实例说明了电化学找矿预测的效果。It has been found that ionic conductivity anomalies in soilcover ofdifferent types of hidden ore deposits are different in character inPinggui area. On the basis of the character of conductivity anomalicsprediction of hidden ore deposits can be conducted. The different typesof hidden ore deposits can be distinguished by these anomalies whichare different in character. This paper explained the results of predic-tion of hidden ore deposits by using the electrochemical method.

关 键 词：钨矿床 锡矿床 隐伏矿床 地化勘探 

分 类 号：P632.2[天文地球—地质矿产勘探]