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Abstract
The main features of the transformation of organic matter (OM) of three facies of metamorphism (the facies of green shales, amphibolite and granulite facies) on the example of the Ukrainian crystal shield are discussed. The area of distribution and content of OM in high-carbon ancient rocks is characterized, the composition of primary sedimentary rocks, the processes of accumulation of biophilic elements during the transformation of OM are reconstructed.
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