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The article considers the classification affiliation and real features of the subvolcanic rocks of the shadoronsky (J2-3) and abagatuysky (K1) complexes of the northern frame of the Borschovochny ridge. This structure is part of the Aga terrain of the Mongol-Okhotsk fold belt. It is established that in the given territory the rocks of the shadoronsky complex are localized in dynamometamorphic formations, and the rocks of the abagatuysky complex in riftogenic depressions. On the basis of mineralogical-petrographic ...