In the present contribution, the copper-noble metal mineralization of the clinopyroxenites of the Shchekurinskiy massif, represented by sulfides of copper and silver, antimonides of palladium, tellurides and arsenides of platinum, as well as native gold, has been studied. Based on the petrographic and petrogeochemical data, the northern portion of the Shchekurinsky massif cannot be related to the other intrusions of the Uralian Platinum belt.