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现代矿业 ›› 2026, Vol. 42 ›› Issue (05): 174-179,186.

• 地质·测量 • 上一篇    下一篇

安徽花园鲁地区铜金钼多金属成矿条件及控矿因素

李永安   

  1. 安徽省地球物理地球化学勘查技术院
  • 出版日期:2026-05-25 发布日期:2026-06-17

Metallogenic Conditions and Ore-controlling Factors of Copper-Gold-Molybdenum Polymetallic Deposits in Huayuanlu Area,Anhui Province

  1. Anhui Institute of Geophysical and Geochemical Prospecting Techniques
  • Online:2026-05-25 Published:2026-06-17

摘要: 安徽花园鲁地区隶属于庐江—滁州成矿亚带,具备良好的铜金多金属成矿潜力。为 查明该区成矿条件与赋矿规律、明确找矿方向,在前人研究基础上,采用地质填图、钻孔编录、水系 沉积物测量及岩矿镜下鉴定等手段,系统分析研究区地质特征。结果表明:区内以震旦系碎屑岩、 碳酸盐岩为主,黄墟组、灯影组为优势赋矿地层,灯影组中段为主要含金层位;黄栗树—破凉亭断 裂及其次级构造为重要控矿构造,马厂复式中酸性岩体为成矿提供物质与热源,构成地层-构造- 岩浆岩耦合控矿体系;区内 Cu、Au、Ag、Mo、Pb、Hg 元素异常北东向展布,浓度分带清晰、套合关系 良好,为典型矿致异常;区内以矽卡岩型铜金矿化为主,斑岩型铜钼矿化次之,矿体多产于岩体接 触带及构造破碎带,矽卡岩化、硅化、黄铁矿化为重要找矿标志。岩浆接触带、断裂交汇部位及化 探异常浓集中心为重点找矿靶区。研究成果可为皖东同类矿床勘查提供参考依据。

关键词: 花园鲁地区, 多金属矿区, 成矿地质条件, 地球化学异常, 控矿因素

Abstract: The Huayuanlu area in Anhui Province belongs to the Lujiang-Chuzhou metallogenic sub⁃ zone,and has good copper-gold polymetallic metallogenic potential. In order to find out the metallogenic conditions and ore-bearing rules in this area and clarify the prospecting direction,on the basis of previous studies,the geological characteristics of the study area are systematically analyzed by means of geological mapping,borehole logging,stream sediment measurement and identification under rock and mineral mi⁃ croscope. The results show that the area is dominated by Sinian clastic rocks and carbonate rocks. The Huangxu Formation and Dengying Formation are the dominant ore-bearing strata,and the middle section of Dengying Formation is the main gold-bearing horizon. The Huanglishu-Poliangting fault and its second⁃ ary structure are important ore-controlling structures. The Machang composite intermediate-acid rock mass provides material and heat source for mineralization,forming a strata-structure-magmatite coupling ore�controlling system. The anomalies of Cu,Au,Ag,Mo,Pb and Hg in the area are distributed in the north⁃ east direction,with clear concentration zoning and good nesting relationship,which are typical ore -in⁃ duced anomalies. The area is dominated by skarn copper-gold mineralization,followed by porphyry cop⁃ per-molybdenum mineralization. The ore bodies are mostly produced in the contact zone of rock mass and tectonic fracture zone. Skarnization,silicification and pyritization are important prospecting indicators. The magmatic contact zone,the intersection of faults and the concentration center of geochemical anomalies are the key prospecting targets. The research results can provide reference for the exploration of similar depos⁃ its in eastern Anhui.

Key words: Huayuanlu area, polymetallic ore field, ore-controlling geological conditions, geochemi? cal anomaly, ore-controlling factors