KARLIN TIPIDAGI APOKARBONAT OLTIN MA’DANLARINING HOSIL BO‘LISH SHAROITLARI
Iles Saidovich OchilovDotsent v.b. (PhD), Qarshi davlat texnika universiteti, Qarshi, O‘zbekistonKuvonchbek Mannonovich UsmonovDotsent, Qarshi davlat texnika universiteti, Qarshi, O‘zbekistonDilrabo Nomozqizi MovlonovaMagistrant, Qarshi davlat texnika universiteti, Qarshi, O‘zbekistonZebo Bahodirqizi BoboqulovaMagistrant, Qarshi davlat texnika universiteti, Qarshi, O‘zbekiston
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In world practice, the issues of forecasting, prospecting, and geological exploration for the discovery of new gold deposits have always been a pressing problem. The great interest in the conditions for the formation of gold mineralization in carbonate rocks is explained by the fact that gold ore deposits in carbonate terrigenous-carbonate formations constitute a significant share of the world's gold reserves. For the formation of gold deposits of the Karlin type, the system of deep faults, formed before ore formation, played the role of channels for the inflow of fluids from the depths.
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