Origin of the Elikanskii granite–gneiss swell in the West Stanovoi terrane of the Central Asian Fold Belt: Results of structural studies

Abstract

Structural studies showed that the Elikanskii granite–gneiss swell is similar to the Late Mesozoic Cordilleran-type metamorphic core complexes distinguished in the southern part of the Eravninskii terrane and in the northeastern part of the Argun–Idermeg superterrane of this belt.