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Tectonostratigraphic investigation shows that the Mesozoic (Triassic–Neocomian) allochthonous terranes of the Anadyr–Koryak accretionary region, from the northwestern continental framing of the Pacific Ocean, form isolated tectonic nappes and slices dispersed all over the region, rather than fragments undeformed paleostructures. Nappes and slices of different stratigraphic horizons, derived from various...
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