The composition and structure of copper containing clays of Gumeshevski copper-scarn field

Gumeshevski Copper-Scarn Field in the Middle Urals is located on the boarder of instrusive and carbon rocks of Devon. It is associated with allochtonous part of strike-slip fault in the zone of bulky split influence, where the metasomatic processes of scarning, propilitization and gold-bearing beresitization, argillization are revealed. Copper containing clays areoccurred during destroying of primary oxidized solids, their transferring and accumulating in the zone of bold Mesozoic karsts. Copper containing clay rocks are aurigerous. They are being reviewed in the range geology-industrial type.