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The  article discusses  the  geological  structure of  the Maksyutovo  complex,  developed  in  the southern part of the Uraltau zone. Particular attention is paid to the carbonaceous deposits widely represented in it (graphitic quartzites, micaceous-graphite-quartz schists). It was shown that they belong to the lowcarbon type and a siliceous-carbon formation. The article notes that the ore-bearing nature of the black shale formation of the Maksyutovo complex is rather weak and is determined by two metallogenic stages. The first is characterized by the predominance of sedimentation processes, and the second is manifested during  the period of  post-sedimentation  activation of  the  region. Manifestations of  phosphorites  are associated with the first one, and pyrite-pyrrhotite-chalcopyrite mineralization with a high gold content is associated with the second one.

Ore prospects of carbonaceous deposits of the Maksyutovo complex (Uraltau zone)