摘要
沿河县丰水岭萤石矿是产于奥陶系湄潭组、红花园组地层中的低温热液型萤石矿,通过对地质特征和成矿模式的分析,认为找矿的主要标志为地层岩性和断裂构造。富集成矿的主要部位为奥陶系湄潭组、红花园组与北西向断裂交汇部位。
Fengshuiling fluorite mine in Yanhe blongs to epithermal fluorite deposite,which originate in Meitan and Honghuayuan group of the Ordovician.By analyzing the geological characteristics and metallogenic model, the main sign of prospecting is identified as formation lithology and falt structure.The main parts of enrichment of ore are the intersection of Meitan and Honghuayuan group of Ordovician and NW faults.
出处
《企业技术开发》
2013年第6期89-91,共3页
Technological Development of Enterprise
关键词
萤石矿
地质特征
成矿模式
fluorite mine
geological characteristics
metallogenic model
