Within Konder ring intrusion during drilling were uncovered bodies of \"ore\" kosvites. It material composition differs sharply from conventional associations of Konder kosvites. Additionally, it contains palladium, silver, platinum, and gold mineralization. On the other hand, the metasomatized alkaline pegmatites mineralization of Konder is unusual. It contain elements, are typical for \"ore\" kosvites (Pb, V, Cu, S) and the contacts of these rocks are often accompanied by a collective recrystallization of the latter. This suggests a link between the processes of formation of alkaline rocks and the mobilization of ore matter (in particular, gold-palladium mineralization) in the ancient pyroxene rocks.