Features of Geological Structure and Mineragenic Specialization of Sheikhdzheyli-Zengiboba of the Sultan-Uvais Ridge Area

The productive mineralization of the Sheikhdzheili-Zengiboba area is associated with metamorphogenic transformations rocks Urusai, Karauzyak, Kuyanchik, Sheikhdzheili suites, metamorphosed under conditions green schist facies. mineralized zones site are confined to narrow faults in tectonic northeast and northwest directions. main form manifestation gold-bearing small steeply dipping veins, lenses, nests, non-extended systems conformal secant quartz veinlets containing dissemination pyrite, arsenopyrite, chalcopyrite pyrrhotite, which represented by gold-arsenopyrite-pyrite, gold-arsenopyrite-chalcopyrite-pyrite natural type ores.