Mineral-morphological peculiarities of auriferous deposits in black schist complexes are determinated by the geodynamic situation for the formation and developing of sedimentary-rock basins. In the shelf surroundings of passive continental outskirts, mainly pelitic and carbonaceous-pelitic black schist complexes with a clearly manifested diagenic stage of lithogenesis are generated. Scale zones of sedimentary-diagenetic sulphides primary enriched with gold are formed as a result. Psammito-aleurite series of sediments are formed by means of avalanche sedimentation in geodynamic surroundings of the foot of a continental slope. This series was turned out under conditions of katagenesis and metagenesis passing the diagenetic stage as a result following the intensive submersion of the basin floor. In spite of all this, quartz veins and vein-streak zones are formed by elizionic processes. These zones are gold-bearing ones under certain lithologo-structural conditions.

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