Metaterrigenous rocks of the Irkut granulite-gneiss Block as indicators of the evolution of the Early Precambrian crust

O. M. Turkina1, Lena Urmantseva1
1Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences, pr. Akademika Koptyuga 3, Novosibirsk, 630090, Russia

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