Abstract
New data about geological structure and composition of magmatic, ore formation and near ore metasomatic changings of complex Karakolskoe deposit of Gorny Altai. The same name stock has zone structure and it composed by two micas granites, with predominance biotites, two micas leucogranites with predominant muscovite, muscovite leucogranites, fine grained two micas leucogranite-porphyres and dike of aplites and alaskites. Rocks of stock submit result of mixed different on composition of melting: calc-alkalic law- aluminum and high-aluminum adakitic with different degrees of partial melting of garnet amphibolites. The tetradic effect of fractionation REE M- type display in rocks. Concentration of beryllium in magmatic rocks rise with increasing of quantity of tetradic effect fractionation REE M-type that it condition transfer of metal by complex compounds of fluor in magmatic fluids. On the isotope of sulfur, carbon and oxygen in minerals set mantle and crust sourcies of ore mineralization. Result in data allow detach magmatic stock in independent Karakolskii granite-leucogranitic complex of Early Triasic age. Ore mineralization occur by quartz-greisen type with beryl, molybdenite, chalcopyrite, pyrite, bismuthinite. Tantalium-niobium ore mineralization disclosed at first. The late type ore mineralization presented by lodes of carbonites with torbernite, metatorbernite and autunite.
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