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Mineralization model for Chahar Gonbad copper-gold deposit (Sirjan), using mineralogical, alteration and geochemical data and multivariate statistical methods
2012
Journal of Economic Geology
The study area is located in southeastern Iran, about 110 km southwest of Kerman. Geologically, the area is composed of ophiolitic rocks, volcanic rocks, intrusive bodies and sedimentary rocks. Vein mineralization within andesite, andesitic basalt, andesitic tuffs occurred along the Chahar Gonbad fault. Sulfide mineralization in the ore deposit has taken place as dissemination, veins and veinlets in which pyrite and chalcopyrite are the most important ores. In this area, argillic, phyllic and
doi:10.22067/econg.v4i1.13397
doaj:913a8438f157411b829a83391d392180
fatcat:b6eseto6wfc3bhqn2f7i2szb3q