RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 19, ES6005, doi:10.2205/2019ES000691, 2019 Figure 1. Scheme of morphostructural zoning (thick lines – lineaments of the I rank, medium – II rank, thin – III rank, solid lines – longitudinal lineaments, dashed – transverse lineaments [Soloviev et al., 2013]), earthquake-prone zones with $M \geq 6.0$ (empty ellipses with blue borders – zones recognized by the "Barrier-3" algorithm, white ellipses – "Cora-3", white ellipses with blue borders – both algorithms) and the epicenters of crustal earthquakes with $M \geq 6.0$ occurred in the Caucasus (Table 1 and Table 3) before 1900 (brown circles), in 1900–1992 (red circles), and after 1992 (green circles). Copyright 2019 by the Geophysical Center RAS. Generated from LaTeX source by ELXfinal, v.2.0 software package. |