摘要
铁路坎矿区属城门山矿区向东延伸部分,矿区露采最低标高为-322m,水文地质条件复杂。通过对有关数据资料的统计分析,从主要含水层、主要构造破碎带、地表水体(赛湖、长江)等方面分析了矿床充水因素。
Tielukan Mining Area belongs to the easterly extension of Chengmenshan copper mining pit.The minimum elevation of open-pit mining is-322 m.The mining conditions of hydrogeology are complex.Through the statistical analysis of the relevant data,analyzing the ore deposit water-filling factor in main aquifer,structural fissures,surface water(Saihu and Yangtze River)and so on.
作者
周祥
高红梅
余金保
ZHOU Xiang;GAO Hong-mei;YU Jin-bao(School of Earth Sciences&Engineering,Nanjing University,Nanjing 210046,China;Northwest Jiangxi Brigade of Jiangxi Province Geology&Minerals Bureau,Jiujiang 332000,China)
出处
《世界有色金属》
2019年第16期166-167,共2页
World Nonferrous Metals
关键词
铁路坎矿区
充水因素
含水层
构造破碎带
地表水体
Tielukan mining area
the factors of filling water
aquifer
structural fracture zone
surface water
