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Metal Mine ›› 2015, Vol. 44 ›› Issue (01): 72-76.

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Study on Process Mineralogy for a Copper Ore in Zambia

Kong Lingcai1,Li Zhengyao2   

  1. 1.Xinxing Development Group Co.,Ltd.,Beijing 100020,China;2.School of Civil and Environment Engineering,University of Science and Technology Beijing,Beijing 100083,China
  • Online:2015-01-15 Published:2015-07-28

Abstract: A certain copper ore in Zambia is a kind of oxidized ore with high proportion of combined phases,in which the grade of copper is 2.10%,and grade of other associated valuable elements such as Fe,Au,Ag,and Co are 24.20%,0.20 g/t,7.60 g/t,and 0.05% respectively.In order to determine the proper beneficiation process,study on process mineralogy of this copper ore was made.The results show that ①the mineral composition is complex and the main useful minerals include hematite-limonite,magnetite,chalcosiderite,green chalcosiderite,pseudo-malachite and so on.②the mineral structures mainly include vesicular,crumby,disseminated granular,riband-striped,circle-like,metacolloform,miarolitic,and veinlet structures,the mineral textures mainly include xenomorphic granular,cryptocrystalline,sarciniform,pectination,columnar and metasomatic.③copper in chalcosiderite,green chalcosiderite and pseudo-malachite account for 41.03%,40.27%,and 15.35% of the total copper respectively.Chalcosiderite and green chalcosiderite are all cryptocrystalline aggregation with particle size of 0.01~0.5 mm.The particle size of pseudo-malachite is generally within the range from 0.01 to 0.4 mm,and few reach up to 0.8 mm.The particle size of hematite-limonite is generally within the range from 0.01 to 0.5 mm,and few reach up to 4 mm.The particle size of magnetite is larger,which is generally within the range from 0.1 to 0.2 mm.Therefore,this kind of copper ore belongs to refractory multi-metal oxidized ore.

Key words: Copper ore, Chalcosiderite, Green chalcosiderite, Pseudo-malachite, Hematite-limonite, Magnetite, Process mineralogy