五指山地区铅锌矿位于川一滇一黔铅锌成矿域东侧,地处紫云—垭都深大断裂以东,是近年来在黔西北地区发现大型铅锌矿产地之一。对黔西北铅锌矿的研究相对集中在垭都—蟒硐、威宁—水城一带,并取得了不少成果,如成矿物质来源(郑传仑,1994;柳贺昌,1996;金中国等2007)、典型矿床特征(唐森宁,1984;欧锦秀,1996;董家龙,2005;金中国,2009;张信伦等2009)、矿床成因(陈士杰,1986)、成矿预测与 The Pb-Zn deposit in the Wuzhishan area is located on the east side of the Yunnan-Yunnan-Yunnan Pb-Zn metallogenic deposit and lies east of the Ziyun-Yaodu fault. It is one of the large-scale lead and zinc deposits found in northwest Guizhou in recent years. The research on the lead-zinc deposits in northwestern Guizhou Province is relatively concentrated in the areas of Yaodu-Python Cave and Weining-Watertown and many achievements have been made, such as the sources of ore-forming materials (Zheng Chuanlun, 1994; Liu Hechang, 1996; Jinzhong et al. 2007) Typical deposit characteristics (Tang Sening, 1984; Ou Jinxiu, 1996; Dong Jialong, 2005; Jin China, 2009; Zhang et al., 2009), genesis of the deposit (Chen Shijie, 1986)