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现代矿业 ›› 2026, Vol. 42 ›› Issue (05): 156-160.

• 地质·测量 • 上一篇    下一篇

某矽卡岩型铜金矿地质特征及找矿预测研究

董来世   

  1. 中国建筑材料工业地质勘查中心黑龙江总队
  • 出版日期:2026-05-25 发布日期:2026-06-17

Study on Geological Characteristics and Prospecting Prediction of a Skarn-type Copper-Gold Deposit

DONG Laishi   

  1. Heilongjiang Corps of China Building Materials Industry Geological Exploration Center
  • Online:2026-05-25 Published:2026-06-17

摘要: 对矿山地质特征进行系统分析是推进区域铜金矿产找矿预测,提升资源利用效率的 关键。以黑龙江省某矽卡岩型铜金矿为研究对象,结合野外地质填图、系统剖面调查、室内岩矿鉴 定及地球化学测试分析等多种方法,系统研究了矿区自然地理与地表特征、区域地层、矿区构造及 岩浆岩、矿区地球化学特征,重点评估了矿石、矿体、围岩的地质特征,在此基础上开展矿床成因分 析与找矿预测研究。研究结果表明,矿区成矿元素富集特征显著,元素富集程度由高到低排序为 As、Sb、Cu、Pb、Zn、W、Ni、Au、Mo、Sn、Ag、Bi,Cu 元素成矿因子达 100.55,Cu、Au 为核心成矿元素;矿 区共圈定 3 条北西向展布的铜金矿化带,区内矽卡岩为弱钙硅酸盐内矽卡岩(SiO2 相对含量 30.72%,Al2O3、Na2O、K2O 总含量 1.06%,Na2O 含量 0.07%);矿床成因以矽卡岩型为主,叠加晚期热 液型矿化,成矿母岩为 109~116 Ma 的花岗斑岩,受地层、岩浆岩、构造三重因素联合控制;矿区 Cu 成矿作用显著,Ⅲ号矿化带规模大,Cu、Au 元素异常强度高,是寻找铜金矿床的理想靶区。研究结 果明确了矿区成矿规律与找矿方向,为区域同类型矽卡岩型铜金矿的勘查与找矿预测提供了理论 指导与实践参考,后续可通过单矿物成分研究查明镓、锗等元素赋存状况,进一步提升矿区资源利 用价值。

关键词: 矽卡岩型铜金矿, 地质特征, 矿床成因, 找矿预测

Abstract: Systematic analysis of mine geological characteristics is the key to promote regional cop⁃ per and gold mineral prospecting prediction and improve resource utilization efficiency. Taking a skarn�type copper-gold deposit in Heilongjiang Province as the research object,combined with various methods such as field geological mapping,systematic profile survey,indoor rock and mineral identification and geo⁃ chemical test analysis,the natural geography and surface characteristics of the mining area,regional stra⁃ ta,mining area structure and magmatic rocks,and geochemical characteristics of the mining area were sys⁃ tematically studied. The geological characteristics of ore,ore body and surrounding rock are evaluated. On this basis,the genesis analysis and prospecting prediction of the deposit were carried out. The results show that the enrichment characteristics of ore-forming elements in the mining area are significant. The order of element enrichment degree from high to low is As、Sb、Cu、Pb、Zn、W、Ni、Au、Mo、Sn、Ag、Bi. The metallo⁃ genic factor of Cu element is 100.55,and Cu and Au are the core ore-forming elements. Three NW-trend⁃ ing copper-gold mineralization belts are delineated in the mining area. The skarn in the area is weak calci⁃ um silicate skarn(SiO2 relative content 30.72%,Al2O3,Na2O,K2O total content 1.06%,Na2O content 0.07%). The genesis of the deposit is mainly skarn type,superimposed with late hydrothermal mineraliza⁃ tion. The ore-forming parent rock is 109~116 Ma granite porphyry,which is controlled by three factors of strata,magmatic rock and structure. The Cu mineralization in the mining area is significant. The Ⅲ miner⁃alization zone is large in scale and the abnormal intensity of Cu and Au elements is high. It is an ideal tar⁃ get area for finding copper-gold deposits. The research results clarify the metallogenic regularity and pros⁃ pecting direction of the mining area,and provide theoretical guidance and practical reference for the explo⁃ ration and prospecting prediction of the same type of skarn copper-gold deposits in the region. In the fu⁃ ture,the occurrence of gallium,germanium and other elements can be identified through the study of sin⁃ gle mineral composition,so as to further improve the utilization value of mining resources.

Key words: skarn-type copper-gold deposit, geological characteristics, ore genesis, prospecting pre? diction