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现代矿业 ›› 2026, Vol. 42 ›› Issue (05): 187-192.

• 地质·测量 • 上一篇    下一篇

刚果(金)Luishia铜钴矿床地质特征和找矿标志研究

王建春 林明明 杨 军 姚 刚 何祖坪 刘宏龙   

  1. 中铁资源集团有限公司
  • 出版日期:2026-05-25 发布日期:2026-06-17

Study on Geological Characteristics and Prospecting Indicators of Luishia Copper-Cobalt Deposit in Congo (DRC)

WANG Jianchun LIN Mingming YANG Jun YAO Gang HE Zuping LIU Honglong   

  1. China Railway Resources Group Co.,Ltd.
  • Online:2026-05-25 Published:2026-06-17

摘要: 刚果(金)Luishia 铜钴矿床位于中非铜钴矿带西延构造单元,成矿条件优越,资源禀 赋良好。为查明矿区地质特征,厘清成矿机制,探明深部及外围资源潜力,在梳理前人研究成果基 础上,综合采用地质填图、高精度磁法测量、激电扫面、钻探工程及岩矿测试等技术手段开展系统 勘查研究。本次勘查采用 100 m×50 m 工程间距,完成 30 个钻孔施工,基本查明矿区地层层序为 RAT、RSF、RSC、SD、CMN、K,其中 SD、CMN 为主要赋矿层位;矿体受褶皱及北西、北东向断裂联合 控制,矿石仅发育氧化矿与硫化矿,无混合矿,氧化矿存在原位氧化与风化淋滤次生富集 2种类型。 研究表明,矿床经历同沉积初始富集、构造变质-热液叠加改造、表生氧化富集三期成矿过程,属典 型的沉积变质-叠加改造层状铜矿床。本次重点对Ⅰ号矿体深部及 C、D 勘查靶区开展工程验证,实 现深部找矿突破,基本查清矿区 11 个矿体的产出特征,重新核定资源储量,有效扩大矿区资源规 模,并系统总结了岩性、构造、矿物、物化探 4 类核心找矿标志,圈定多处磁异常潜力区。研究成果 可为矿区后续勘探开发提供地质依据,亦可为同类铜钴矿床勘查提供参考。

关键词: 铜钴矿床, 地质特征, 矿床成因, 找矿标志, 勘查靶区

Abstract: The Luishia copper-cobalt deposit in Congo (DRC) is located in the western extension tec⁃ tonic unit of the Central African copper-cobalt ore belt,with superior metallogenic conditions and good re⁃ source endowment. In order to find out the geological characteristics of the mining area,clarify the metallo⁃ genic mechanism,and explore the potential of deep and peripheral resources,based on the previous re⁃ search results,this paper comprehensively uses geological mapping,high-precision magnetic measure⁃ ment,IP scanning,drilling engineering and rock and mineral testing to carry out systematic exploration re⁃ search. In this survey,30 boreholes are completed with a project spacing of 100 m×50 m. The stratigraphic sequence of the mining area is basically identified as RAT,RSF,RSC,SD,CMN and K,among which SD and CMN are the main ore-bearing strata. The ore body is controlled by folds and NW and NE trending faults. The ore only develops oxidized ore and sulfide ore,and there is no mixed ore. The oxidized ores are divided into in-situ oxidized type and weathering-leaching secondary enrichment type. The deposit has ex⁃ perienced three metallogenic stages,including syndepositional initial enrichment,tectonic metamorphic�hydrothermal superimposed reformation,and supergene oxidation enrichment,and belongs to a typical sedimentary-metamorphic and superimposed stratiform copper deposit. This paper focuses on the engineer⁃ ing verification of the deep part of No.I ore body and the exploration target areas of C and D,realizes thebreakthrough of deep prospecting,basically finds out the output characteristics of 11 ore bodies in the min⁃ ing area,re-approves the resource reserves,effectively expands the resource scale of the mining area, and systematically summarizes the four core prospecting indicators of lithology,structure,mineral and geo⁃ physical and geochemical exploration,and delineates many potential areas of magnetic anomaly. The re⁃ search results can provide geological basis for the subsequent exploration and development of the mining ar⁃ ea,and can also provide reference for the exploration of similar copper-cobalt deposits.

Key words: copper-cobalt deposits, geological characteristics, deposit genesist, prospecting indica? tors, exploration target