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现代矿业 ›› 2026, Vol. 42 ›› Issue (02): 198-202.

• 地质·测量 • 上一篇    下一篇

刚果(金)利卡西—康波夫矿集区Lujiba铜钴矿地质特征及找矿标志

刘路全 沈忠义 管力瑶 刘 坚   

  1. 中国有色金属工业昆明勘察设计研究院有限公司
  • 出版日期:2026-02-25 发布日期:2026-03-17

Geological Characteristics and Prospecting Markers of the Lujiba Copper-Cobalt Deposit in the Likasi-Kompov Mining Concentration Area of the Democratic Republic of the Congo

  1. Kunming Prospecting Design Institute of China Nonferrous Metals Industry Co.,Ltd.
  • Online:2026-02-25 Published:2026-03-17

摘要: Lujiba 铜钴矿床隶属于刚果(金)—赞比亚成矿域的加丹加铜-钴成矿带,该区经历了 多期次的构造-推覆运动,形成了复杂的构造格局,并伴随着大量层状、似层状矿床的产出。矿床 主要赋存于加丹加超群下部的罗安群碎屑岩-碳酸盐岩建造中,具有显著的层控特征。为查明矿 床成矿规律及阶段,对区域成矿特征、矿床地质特征进行详细分析,系统厘定了矿石矿物特征及找 矿标志。结果表明:矿(化)体主要产于罗安群矿山组 R2 硅质白云岩、砂质白云岩中,呈层状、似层 状产出;矿区构造继承了区域构造特征,褶皱构造及同期的走向断裂控制着含矿层位的空间分布, 后期形成的次级构造为含矿热液提供运移通道及容矿空间,矿(化)层严格受层位及构造控制;矿 床中矿石矿物主要为孔雀石、辉铜矿,含少量自然铜、斑铜矿、赤铜矿等,矿床成矿期可划分为初始 成矿期、主成矿期、热液改造期及表生富集期 4 个阶段;Lujiba 铜钴矿床是经过多次构造、热液叠加 改造及变质改造作用的层控型矿床,地层岩性、构造、典型矿物等标志特征都是同类矿床的找矿标 志。

关键词: 铜钴矿, 地质特征, 成矿阶段, 找矿标志

Abstract: The Lujiba copper-cobalt deposit is located in the Katanga copper-cobalt mineralization belt within the Congolese(DRC)- Zambia mineralization domain. This area has undergone multiple stages of tectonic-overlying movements,forming a complex tectonic pattern and accompanied by the occurrence of a large number of layered and quasi-layered deposits. The deposit is mainly located in the Luo′an Group clastic rock-carbonate formation in the lower part of the Katanga Supergroup and has significant layer-con⁃ trolled characteristics. To clarify the metallogenic regularity and stages of the deposit,through a detailed analysis of the regional metallogenic characteristics and geological features of the deposit,the mineral char⁃ acteristics of the ore and the prospecting indicators were systematically determined. The results show that the ore (mineralized) mainly occurs in the R2 siliceous dolomite and sandy dolomite of the Luo ′an Group mining group,and is produced in layered and quasi-layered forms. The mining area structure inherits the regional structural characteristics. The folding structure and the concurrent strike faults control the spatial distribution of the ore-bearing strata. The secondary structures formed later provide migration channels and ore-bearing space for the ore-bearing hydrothermal fluid. The ore - (mineralized) strata are strictly con⁃ trolled by the strata and structure. The main ore minerals in the deposit are malachite and chalcocite,with a small amount of natural copper,porphyrite,chalcocite,etc. The mineralization period of the deposit can be divided into four stages of the initial mineralization period,the main mineralization period,the hydro⁃ thermal modification period and the surface enrichment period. The Lujiba copper-cobalt deposit is a lay⁃ er-controlled deposit that has undergone multiple tectonic,hydrothermal superposition and metamorphic modifications. The lithology,structure,typical minerals and other characteristic features of the strata are all exploration indicators for similar deposits.

Key words: copper-cobalt deposit, geological characteristics, metallogenic stage, prospecting mark? ers