Geochemical peculiarities of carbonaceous shalesThe ore-enclosing strata in the Kumak field represent mostly carbon-bearing siltstone and carbonaceous-clayey shale. The elemental composition features the increased contents of MgO (0.60-6.42%), TiO 2 (0.29-1.89%) and Al 2 O 3 (9.40-31.50%), and, accordingly, the increased hydrolyzate module (>0.55 units) and alumosilicic module (0.77 units, average 0.38 units). Lithochemically, they conform with siallite and super aluminum hydrolyzate rocks associated with residuum and including high percentage of volcanogenic material [19]. Highrepeatability chemical indexes of alteration (CIA = 100Al 2 O 3 / (Al 2 O 3 + UDC 553.41