ГЕОМОРФОЛОГИЯ И МОРФОТЕКТОНИКА ЛЕНО-АНГАРСКОГО ПЛАТО

Abstract

Lena-Angara plateau occupies the central part of the southern projection of Siberian platform. The young uplift of plateau has non-arched character. Its cause is the accretion of layered rock masses of platform cover, detached sub-horizontally by evaporates layers. Typta-Tutur depression has a peculiar position in the young tectonics of plateau, being the reversed-straighl morphostucture.