Skarn-related gold-copper mineralization of the Baranchinskaya area (Gornyi Altai)
DOI:10.47765/0869-7175-2025-10007
Keywords:
Gornyi Altai, Barancha, gold, skarns, axinite, datolite, okayamalite, fluid inclusionsAbstract
The composition and sequence of formation of skarn-related gold-copper mineralization of the Baranchinskaya area have been determined. The pyroxene-garnet skarns are intensely replaced by boron-containing vesuvianite that in turn is replaced by borosilicates in paragenesis with gold-sulfide mineralization. The borosilicates are represented by tourmaline, axinite, and datolite, as well as by okayamalite first found in Russia. Ore minerals are mainly represented by chalcopyrite, bornite, wittichenite, native bismuth, and electrum. The ore mineralization was formed by alkaline-chloride solutions in the temperature range of 385-330 °C at a pressure of about 1000 bar. The Karagu deposit in the Gornyi Altai is considered as the closest analogue.