RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 17, ES1002, doi:10.2205/2017ES000590, 2017
Figure 8. The secondary disturbances of Karahem depression and its vicinity. A – the vibrational fracture in the rocky ground of the proluvial trail (6 in Figure 2); B – the rockfall at the slope of the Chas-Tayga ridge (12 in Figure 2); C – the rockfall at the slope of the watershed (9 in Figure 2); D – the slideslip of the slope cover (10 in Figure 2).
Citation: Ovsyuchenko A. N., E. A. Rogozhin, A. V. Marakhanov, Yu. V. Butanaev, A. S. Larkov, S. S. Novikov (2017), Environmental effects of the 2011–2012 Tuva earthquakes (Russia): Application of ESI 2007 macroseismic scale in the Siberian mountains, Russ. J. Earth Sci., 17, ES1002, doi:10.2205/2017ES000590.
Copyright 2017 by the Geophysical Center RAS.
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