Abstract
Based on the peculiarities of gold manifestations in carbonaceous schists of the Southern Urals, a model for the genesis of gold mineralization is proposed. The pattern takes a complex of related processes into consideration: sedimentation, transformation as a result of submergence, dynamometamorphism, and contact metamorphism. Hence, prognostic-prospecting factors for searching for the hydrothermal-metamorphogenic gold mineralization in carbonaceous deposits are proposed.
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