The analysis of statistically representative material of lithochemical sampling within Veresoborsky dunite massif revealed a group of correlating chemical elements (Cr, Mn, Co, Ni, Bi, Sn, W, Zn) whose accumulation trend coincides with that of Pt. The established pattern enables proposing criteria of comparative evaluation regarding primary Pt mineralization productivity of local areas (0,5-3 km2) in both Veresoborsky massif and its counterparts composed of the Urals Kachkanarsky complex (υO3k) rocks.