Geodynamic conditions of the formation of the Badiayu and Yarot massifs (the Subpolar Urals)

Abstract

The study of high-potassium medium-grained leukogranites of the Badiayu and Yarots massifs (the Subpolar Urals), which break through the deposits of the Moroinsky formation, allowed not only to confirm L. V. Makhlaev's assumption of early belonging to a single pluto, but also on the basis of a comprehensive study of petrogenic and rare elements using qualification diagrams to establish that the formation of the studied rocks is associated with the post-collisional stage of development Protouralid is a Timanid.