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This analysis reveals the structure and complexity of dynamometamorphic complexes in the Yenisei Ridge, suggesting a new model for regional geology.
A new approach has been developed to analyze the geology of the Yenisei Ridge based on the revision of the role of geodynamic factors. The complexes of dynamometamorphic rock assemblages are recognized as an independent class of objects comparable in scale to the known massifs of sedimentary or magmatic formations. The Late-Riphean Shumikha and post Vendian (Late Paleozoic ?) Tyryda dynamometamorphic complexes with specific diagnostic features are distinguished and justified. Based on the results of mapping these structures, a new understanding of regional structure has been obtained as a model of megamelange of the thrust-overthrust type where lenticular-tabular blocks of heterogeneous nature are separated by netlike zones of the Tyryda dynamometamorphic complex.
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S.V. Goryainov (1993) studied this question.
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