In recent years, numerous quartz and carbonate-quartz veins with polymetallic mineralization have been identified in the north of the Taimyr-North-Earth folded region within the Mininsko-Bolshevist myogeosynclinal structural-formation zone.

Since the 70's in the north of the Central Taymir, considerable attention has been paid to quartz and carbonate-quartz veins with polysulfide mineralization, which is due to the isolation in the Taymir quartz (sulfide)-gold ore formation.