MORPHOSTRUCTURE OF THE KODAR-UDOKAN SECTION OF THE BAIKAL RIFT ZONE
The morphostructure of the region is a natural result of active geodynamics in the eastern Stanovoe Upland. Extreme seismic conditions become apparent in rare devastating earthquakes (up to 10-11 in the Mercally scale), as well as in frequent slight ones. Seismic events affect topography and produce...
Main Authors: | , |
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Format: | Article |
Language: | English |
Published: |
Lomonosov Moscow State University
2014-03-01
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Series: | Geography, Environment, Sustainability |
Subjects: | |
Online Access: | https://ges.rgo.ru/jour/article/view/57 |