摘要
对六苴铜矿小河-石门坎矿段水文地质、工程地质及环境地质进行了系统详细的调查研究,研究结果表明:调查区矿床为以裂隙含水层充水为主的矿床。矿床充水强度不大,属富水性弱的矿床。小河-石门坎矿段矿床岩体稳定性较好,矿床工程地质复杂程度较为简单。调查区及矿床开拓区环境地质灾害不发育,属地质环境质量不良矿区。地质调查研究为矿山小河-石门坎矿段未来整体工程建设布置及矿床开采方法确定提供了参考依据。
Based on systemic and detailed survey research on hydrological geologic, engineering geologic and environmental geologic of Xiaohe-Shimenkan ore block of Liuju copper mine, The study results show survey area ore deposit was cranny hydrated stratum. Water-filling intensity of ore deposit was weak. It belonged weak water characteristic ore deposit, mass stability of Xiaohe-Shimenkan is better, geologic complication-degree was simple. Environmental ge-hazards of survey area and ore deposit exploiting area didn't obviously develop. It can afford reference warranty for future whole engineering lay and ore deposit miningmethod option.
出处
《中国矿业》
北大核心
2008年第6期87-90,共4页
China Mining Magazine
关键词
水文地质
工程地质
环境地质
地质调查
hydrological geologic
engineering geologic
environmental geologic
geological survey