THE MORPHOLOGY OF MINERALS OFTHE MINE YANGI DОVON AND ITS MINERALOGICAL COMPOSITION OF MOUNTAIN ROCKS INCLUDING THEM

Аннотация

In Yangi Dоvon, all faults relate to the three age groups: to the upper Carboniferous, pre-Permian and Permian. The deep fault to the upper Carboniferous age has been separated into the Karakutan fault zone with a length of more than 30 km and a width of 2-3 km. Within its borders there are three branches, Karakutan, Kyzbibinskaya and Severnaya, which play a leading role in the distribution of gold mineralization. They represent weakened zones of fragmentation and changes, consisting of smaller parallel and intersecting violations with numerous crevices of the northeast and northwestern strike.