Abstract
The article presents data summarization on magmatism and metamorphism of the Kanin-Timan-Pechora region and spatial analysis of the distribution of endogenous processes products in Late Proterozoic — Early Cambrian. A concentrated localization of the products of two mantle plumes, which gave rise to igneous complexes and relatively high-temperature regional metamorphism, was revealed in “Northern” and “Southern” areas separated from each other by an amagmatic area 250—300 km long with a relatively low level of regional metamorphic transformation of sedimentary rocks.
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