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《Geotectonica Et Metallogenia》 2011-01
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Geochemistry of the Brwons Co-Cu-Ni Polymetallic Deposit and Comparison with the Black Shale Hosted Polymetallic Deposits in South China

WANG Mingyan1,2,WANG Anjian1,DENG Shengfu2,LIU Wei2 and ZHANG Dexian3(1.Institute of Mineral Resources,Chinese Academy of Geological Sciences,Beijing 100037; 2.Department of Mineral Resources,HNG,Changsha 410015,Hunan,China; 3.School of Geosciences and Environmental Engineering,Central South University,Changsha 410083,Hunan,China)  
The Browns Co-Cu-Ni deposit is hosted by the Whites Shale of Paleo-Preterozoic in Northern Territory of Australia,and it is a typical strata-bound deposit. Based on the analysis of the geological characters in detail,the major elements,trace elements,Pb and S isotope,and the organic matter,the enrichment mechanism of the ore metals is studied in this paper. The main Co-hosting mineral is siegenite,which is carried by pyrite. δ34S values of the sulfides range from-5.21‰ to +14.78‰,indicating involvement of thermochemical reduction and bacterial activity. Homogeneous lead isotope features of galena (206Pb/204Pb=16.20~16.22,207Pb/206Pb= 15.48~15.51,208Pb/207Pb=35.86~35.92) suggest that Pb was derived from the crust. Ore geochemical studies illustrate that the deposit is primarily of sedimentary origin and were somewhat reformed by later tectonic-thermal events. Compared with the deposits hosted in the South China black shales,it can be concluded that the Browns deposit is a normal sedimentation deposit,while the latter are Sedex-type deposits.
【Fund】: 国土资源部“2008年度境外矿产资源风险勘探财政补贴”项目;; 国家科技攻关计划课题(编号2003BA612A-05)
【CateGory Index】: P618.2
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