摘要
云南镇康县小干沟金矿为石英脉型金矿,金矿体主要产于上三叠统牛喝塘组玄武岩之构造破碎带中。该矿床的成矿条件和地球化学特征表明,小干沟金矿的矿化元素具有明显的分带性,地表浅部以金为主,中深部出现钨、铜、铅锌等多金属矿化,显示了该矿具有较好的找矿前景。
Xiaogangou Au deposit is a quartz vein Au deposit. The ore body is mainly in the structural fracture zone of Upper Triassic basalt. The metallogenetic conditions and geochemical feature show the clear zonation of metallogenetic element of Xiaogangou Au deposit, surface mainly Au, middle-deep w, Cu Pb-Zn, etc muhimetallic metallogenesis, with good prospecting potentiality.
出处
《云南地质》
2016年第2期209-213,共5页
Yunnan Geology
关键词
构造控矿
元素分带
热液型矿床
云南镇康小干沟
Ore Control of Structure
Element Zonation
Hydrothennal Deposit
Xiaogangou, Zhenkang,Yunnan
