RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 17, ES1002, doi:10.2205/2017ES000590, 2017 Figure 5. The seismic rupture of the second Tuva earthquake on 26.02.2012. A – The upthrust–overthrust responsible for the elevation and drying of the swamped before land; B – The frazil clogging by sand in the sunken flank of the seismic rupture. Behind the seismotectonic scarp is seen. Copyright 2017 by the Geophysical Center RAS. Generated from LaTeX source by ELXpaper, v.1.5 software package. |