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Abstract
On the basis of the study of Early Precambrian metamorphosed volcanogenic-sedimentary rocks of the Vyatka belt of the northeastern Volga-Ural megablock, East European craton, the report will consider the tectonic setting of the formation of this belt and its place in the paleocontinental correlations 2.2-2.0 Ga ago.
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Schedule a callMore From: Proceedings of the Karelian Research Centre of the Russian Academy of Sciences
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