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The article presents a review of own and published data on orebearing of mainly granitoid and ultrabasic massifs of the Bashkirian meganticlinorium, Zilair magasynclinorium, Uraltau meganticlinorium and the zone of the Main Uralian fault. It is shown that the greatest prospects for gold mineralization among the granitoid intrusions of the Bashkirian meganticlinorium has a framing of Akhmerovsky massif, which is part of the Beloretsky metamorphic complex, on the periphery of which in carbonaceous deposits revealed a number of gold manifestations. All of them are confined to the external high-temperature zone of green shale facies of metamorphism. Within Zilair megasynclinorium the largest and almost the only is the gabbro-

ORE-BEARING OF INTRUSIVE COMPLEXES IN THE NORTHERN PART OF THE WESTERN SLOPE OF THE SOUTHERN URALS