RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 17, ES1002, doi:10.2205/2017ES000590, 2017
Figure 3. The seismic rupture of the first Tuva earthquake on 27.12.2011. A – "Scouring" strike-slip rupture on the slope of watershed; B – strike-slip rupture in the valley of the stream; C – normal fault – strike-slip rupture on the western limitation of the saddle-graben; D – normal fault – strike-slip rupture on the eastern limitation of the saddle-graben.
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.
Generated from LaTeX source by ELXpaper, v.1.5 software package.