摘要
李村铅锌矿地处四川省攀西铅锌矿集区,是会理地区重要的铅锌矿远景区之一。李村远景区具有良好的地质成矿条件——挤压断裂带及褪色蚀变带,电吸附地球化学测量呈现浓集中心明显的Cu、Pb、Zn、A g组合异常,并沿挤压断裂带及褪色蚀变带呈面状、团块状分布,与地表发现的Pb、Zn矿化吻合,为进一步找矿工作指明了方向。
Licun Pb-Zn deposit is located at the deposit concentration mine,one important potential area of Pb-Zn deposit in the Huili region,Panxi,Sichuan province.There are favorable geological and mineralized conditions,extrusion fault belt and fading alteration belt.By geochemical method of electronic adsorption there appears Cu-Pb-Zn-Ag assembled anomaly with obvious dense centers,which are along extrusion fault belt and fading alteration belt as plane and conglomeration shape.It is inosculated with the mineralization in the surface. The exploration direction is pointed out for the future work.
出处
《矿产与地质》
2009年第3期268-272,共5页
Mineral Resources and Geology
基金
广西自然科学基金项目(桂科自0640181)资助
关键词
铅锌矿
地球化学特征
电吸附
找矿前景
攀西李村
Pb-Zn deposit
geochemical feature
electronic adsorption
prospecting potential