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黄沙坪铅锌多金属矿是南岭成矿带典型的铅锌多金属矿床,矿床位于东西向南岭成矿带与北东向钦杭成矿带交汇的湘南地区,是危机矿山接替资源勘查项目执行以来取得重大突破的矿床之一。矿床成矿地质条件优越,历来为众多的地质工作者所瞩目,研究程度较高。近年来许多学者对矿床的成矿时代做了大量的研究,获得钨钼矿体辉钼矿Re-Os年龄为154~159 Ma(马丽艳等,2007;毛景文等,2007;姚军明,2007;雷泽恒等,2010),但对铅锌矿体仍缺乏精
The Huangshaping Pb-Zn polymetallic deposit is a typical Pb-Zn polymetallic deposit in the Nanling metallogenic belt. The deposit is located in the southern Hunan region where the east-west Nanling metallogenic belt intersects with the northeast Qinhuang metallogenic belt, Since the implementation of the project has made a major breakthrough in one of the deposits. Mineralization geological conditions are superior, has always been the focus of many geological workers, a high degree of research. In recent years, many scholars have done a great deal of research on the mineralization age of the deposit. The Re-Os age of the molybdenite of the tungsten-molybdenum ore body is 154-159 Ma (Ma Liyan et al. 2007; Mao Jingwen et al. 2007; Yao Junming 2007; Lei Ze Constant, 2010), but the lack of refined lead-zinc ore body