Abstract
Issues pertaining to the genesis of massive sulfide deposits (Kizil Dere and others) embedded in Jurassic black shales of the eastern Caucasus are discussed on the basis of field materials. Major structural-dynamic constraints along with structural, lithological, and mineralogical indicators of the formation of such deposits have been established. These deposits are epigenetic objects formed during active deformations of clayey sequences and migration of metagenic waters over sources of deep ore-conducting fractures in structural and other traps. Therefore, they can be referred to the metagenic-hydrothermal type.
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