rily,thegenesis ofepithermaldepositormagmatichydrothermaldeposithasnotbeenpaidenoughattentions.Inrecentyears,thelarge scaleXiongcuncopper—golddeposit,discoveredinthemiddleoftheGangdiseMountains,isregardedasmagmatic hydrothermaltype.Luobuzhencopper—polymetallicdepositisalsolocatedatmiddleoftheGangdiseMountains,whichis neartoXiongcunoredistrict.Inthispaper,onthebasisofanalysisongeologicalcharacteristics,orebodyandore paringitsgenesiswithXiongcuncopper—golddeposit,itisconcludedthatthe genesisofLuobuzhendepositbelongstomagmatichydrothermalalteredtype.Takingitasacasestudy,theauthors furtherdeducethemetallogenyinthemiddleGangdise,whichprovidestheneWideaofprospectingintheGangdise metallogenicbelt. KeyWords:Tibet;Luobuzhen;geologicalcharacteristics;magmatichydrothermalsolution;genesisanalysis 维普资讯
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