Abstract
A detailed classification of regional metamorphic rock facies is presented along with the results of compiling a small scale Map of Metamorphic Facies of U.S.S.R. It is demonstrated that typical metamorphic complexes are associated with certain large structural elements of the crust. The aspects of metamorphism are used in identifying the areas of ancient platforms, two types of mobile belts, and two types of high pressure zones at the junction of major structures of different degrees of stability.—Author
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