摘要
长流水金矿床矿体主要受断裂控制,含水岩组主要为基岩裂隙水和断裂破碎带,为裂隙充水矿床,矿床水文地质条件类型属简单类型;矿区地下水为SO42-—Cl-—Na+—Ca2+型水,水质差且具中等腐蚀性,不能作为生活饮用水,也不能作为工业锅炉用水。
The orebody of the Changliushui gold deposit is mainly controlled by faults.The water-bearing rock group is mainly bedrock fissure water and fracture zone.It is a fissure-filled deposit.The type of hydrogeological conditions of the deposit is a simple type.The groundwater is SO42-—Cl-—Na^+—Ca^2+water in the mining area.Groundwater quality difference and having a corrosive medium,.It cannot be used as domestic drinking water and industrial boiler water.
作者
唐艳
刘佳海
TANG Yan;LIU Jia-hai(Zhangye Geo-mine Survey Instisute of Non-frerous Metal Geological Exploration of Gansu Province,Zhangye 734012,China)
出处
《世界有色金属》
2020年第3期139-140,共2页
World Nonferrous Metals
关键词
水文地质
水质
长流水金矿床
甘肃
hydrogeology
water quality
changliushui gold deposits
gansu