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浙江平水铜矿是浙江省最大的铜矿床,为典型的火山成因块状硫化物矿床(VMS),其位于钦杭成矿带北东段浙西北地区。平水铜矿已连续开采了30余年,目前属于危机矿山。前人对平水铜矿在地质特征、成矿流体、矿床成因及成岩成矿年代学等方面已经进行了大量、详细的研究(Chen et al.,2015),但主要集中在矿床成因等方面;而在矿床勘查方面研究依旧薄弱,亟需开展以找矿预测为目的的相关
Zhejiang Pingshui copper deposit is the largest copper deposit in Zhejiang Province. It is a typical volcanic-generous massive sulfide deposit (VMS) located in the north east Zhejiang Province of the Qinhang metallogenic belt. Pingshui copper mine has been continuously mined more than 30 years, is currently a crisis mine. The predecessors have conducted extensive and detailed studies on the geological characteristics, ore-forming fluids, genesis and diagenetic metallogenic chronology of Pingshui copper mine (Chen et al., 2015), but mainly focused on the genesis of the deposit. However, research on deposit exploration is still weak and there is an urgent need to carry out the exploration for the purpose of prospecting