“…This orebody is distinguished from the Main orebody by much higher Pb and BaSO 4 grades at a similar Zn grade. At the same time, it should be admitted that ore mineralization in ERSs and the localization of the Main orebody at the flank of the tectonic suture are particular and the most favorable local manifestations of a typical ore-controlling combination of fault and ore-bearing stratigraphic unit common to the Kuzha ore field and some other districts with stratiform base-metal mineralization (Heyl, 1968;Bogashova, 1987). The crosscutting faults with open cavities (relaxation fissures surrounding ERSs pertain to exactly this type of faults) made mixing of water from different levels possible, and this, in turn, led to the leaching of heavy metals from sedimentary rocks and clastic grains by chloride solutions and the subsequent precipitation of Fe, Pb, and Zn on hydrogen sulfide barriers.…”