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刚果(金)如瓦西铜-钴矿床表生成矿过程及其勘探意义

陶玻 王涛 李昶 贾宗明 白发青 薛明 田毓龙 邱正杰

地质与勘探2024,Vol.60Issue(3):631-642,12.
地质与勘探2024,Vol.60Issue(3):631-642,12.DOI:10.12134/j.dzykt.2024.03.018

刚果(金)如瓦西铜-钴矿床表生成矿过程及其勘探意义

Supergene Metallogenesis and Its Prospecting Significance of the Ruashi Cu-Co Deposit in D.R.Congo

陶玻 1王涛 1李昶 1贾宗明 1白发青 1薛明 1田毓龙 2邱正杰3

作者信息

  • 1. 金川集团股份有限公司,甘肃金昌 737100||梅特瑞斯如瓦西矿业公司,刚果(金)卢本巴西 20043
  • 2. 金川集团股份有限公司,甘肃金昌 737100
  • 3. 中国科学院地质与地球物理研究所,北京 100029
  • 折叠

摘要

Abstract

The Ruashi copper-cobalt deposit in the Central African Metallogenic Belt has undergone supergene oxidation and secondary enrichment,but the related research is weak.This work analyzed the composition of supergene zoning and its metallogenesis based on geological surveys,mineralogical observations and production resource exploration of this deposit.The primary orebodies contain sulfide minerals of chalcopyrite,bornite,chalcogenite,and the ore grade ranges in 1%~2%for copper and 0.1%~0.3%for cobalt.The upper oxidation belt can be further divided into three sub zones,i.e.,the complete oxidation subzone,the leaching subzone and the secondary oxide enrichment subzone.The complete oxidation subzone develops the"gossan"with cobalt-rich oxide accumulation(cobalt grade is 1%~3%,locally reaching up to 12%).The leaching subzone contains almost no copper and cobalt metal minerals.The secondary enriched oxide subzone includes oxide minerals of malachite,silicomalachite,azurite,chalcopyrite,and water chalcopyrite,as well as carbonate minerals.The ore grade is 5%~10%for copper and 0.8%~1.0%for cobalt,which is enriched by 3~5 times than the primary ore.The lower part is the secondary sulfide enrichment including chalcopyrite and chalcocite.The ore grade is within the range of 3%~5%for copper and 0.3%~0.8%cobalt,which is 1~3 times enriched than the primary sulfide ore.The study reveals that the Ruashi deposit has experienced multi-period and multi-stage metallogenic evolution,and the supergene oxidation zoning is controlled by factors such as rock stratum,geological structures,and groundwater.The secondary enrichment has significantly improved the ore grade and development value,which formed high to ultra-high grade ore bodies such as the Cu-Co-enriched oxide ore,Cu-Co-enriched sulfide ore,Cu-enriched oxide ore near the contact zone of carbonate rock and black Co-enriched ore.Exploration indicates that the newly discovered high-grade ore resources in the deep edge of the deposit are 2.56 million tons,with an average grade of 3.68%copper and 0.44%cobalt.The recoverable reserves are 1.43 million tons,with an average grade of 3.53%copper and 0.32%cobalt.This study can provide scientific basis for the epigenetic enrichment of sulfide deposits evolving into oxide deposits in the same type of mines and region,as well as for deep edge exploration prediction.

关键词

表生氧化/次生富集/找矿预测/高品位矿石/如瓦西铜-钴矿床/刚果(金)

Key words

supergene oxidation/secondary enrichment/prospecting prediction/high-grade ore/Ruashi Cu-Co deposit/D.R.Congo

分类

天文与地球科学

引用本文复制引用

陶玻,王涛,李昶,贾宗明,白发青,薛明,田毓龙,邱正杰..刚果(金)如瓦西铜-钴矿床表生成矿过程及其勘探意义[J].地质与勘探,2024,60(3):631-642,12.

基金项目

金川集团股份有限公司如瓦西铜钴矿科技项目(编号:JKCCnull2019003)资助. (编号:JKCCnull2019003)

地质与勘探

OA北大核心CSTPCD

0495-5331

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