摘要
将激电测深法应用于青海省查查香卡地区多金属矿勘查,根据测量结果圈定异常的埋深、产状等,并查清了测区多金属矿构造蚀变带的位置,经后期钻孔验证,见矿情况和异常基本吻合。认为激电测深异常推测的构造蚀变带及矿化带,与多金属成矿关系密切。该方法的应用对地质条件类似地区多金属找矿工作具有一定的参考作用。
Induced polarization sounding method was used to prospect poly-metallic deposit in Chachaxiangka Area of Qaidam Basin in Qinghai.The measured data can delineate the depth and occurences of the anomaly and identify the geological structure and alteration which were validated with later drilling.Therefore,the method was considered to be effective in deducing the structual and alteration zone related to mineralization and can provide useful information to guiding the poly-metallic prospecting in similar area.
出处
《铀矿地质》
CAS
CSCD
2015年第6期600-605,共6页
Uranium Geology
关键词
激电测深法
多金属矿
硫化物
硅化蚀变带
induced polarization sounding method
poly-metallic ore
sulphide
silicified alteration zone