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红透山铜锌矿床是我国地质年代最老的块状硫化物铜矿床。前人对其研究也非常深入和全面,涉及矿床成因研究(张雅静,2010)、深部及外围找矿预测研究(魏有惠等,2010)、伴生矿物赋存状态研究(单连军,2009)、探采对比研究(赵刚等,2010)、控矿因素研究(赵刚等,2010)、找矿标志研究(翟明国,1985)等方面。本文主要从矿石工艺学方面对该矿床进行研究,为研究矿床成矿机制和找矿预测提供一定的依据。
The Hongtoushan copper-zinc deposit is the oldest massive sulphide copper deposit in China. The predecessors’ research on them is also very thorough and comprehensive. They involve the study of the genesis of the deposit (Zhang Yajing, 2010), the prediction of deep and peripheral ore prospecting (Wei Youhui et al., 2010), the study of the occurrence of associated minerals (Shan Lianjun, 2009) Mining comparison (Zhao et al., 2010), research on ore-controlling factors (Zhao Gang et al., 2010), research on prospecting markers (Zhai Mingguo, 1985) and so on. This article mainly studies the ore deposit from the aspect of ore technology and provides some evidences for studying the ore-forming mechanism and prospecting prognosis.