MORPHOSTRUCTURE OF THE SIBERIAN PLATFORM
https://doi.org/10.15356/0435-4281-1971-1-11-23
Abstract
The main peculiarities of the recent mophostructure of the Siberian Platform are considered to be the result of a complex interaction of crystalline base blocks, which irregularly moved in the Mezosoic and Cenozoic Eras. They are grouped into semicircle zones of direct, reversed, and complex morphostructures, which have undergone wave-like movements of a planetary character. The blocks form a framework of submeridional and northeast directions.
Review
For citations:
Adamenko O.M. MORPHOSTRUCTURE OF THE SIBERIAN PLATFORM. Geomorfologiya. 1971;(1):11-21. (In Russ.) https://doi.org/10.15356/0435-4281-1971-1-11-23
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