On an example of the Urals using the materials of the other regions the geodynamic conditions of vol-canogenic sulfide deposits formation at the stages of divergence and convergence of fold systems have been considered. At the first stage sulfide deposits are formed in conditions of continental grabens (Filizchay type), MOVR, over island arcs and island arcs rifts (Cyprus type), oceanic grabens (Besshi type). At the stage of convergence of fold belts the main factor of ore-bearing volcanic formations and sulfide deposits is a subduction of some crustal blocks under others. The Urals and Baimak type sulfide deposits are formed in oversubduction zones of oceanic crust sinking under oceanic one in conditions of ensimatic island arcs. The Malokavkaz and Kuroko types sulfide deposits are generateed over zones of oceanic crust subduction under continental one in conditions of ensimatic island arcs. The Iberian type deposits are formed over subduction zones of continental crust under continental one.