RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 14, ES2005, doi:10.2205/2014ES000542, 2014

Figure 2. Elements of basement tectonics by [Kirs et al., 2009; Koistinen et al., 2001; Korsman et al., 1997; Sharov et al., 2007; Vaisanen and Skytta, 2007]. Basement units: I, Estonian-Latvian granulite belt; II, South Estonian Zone; III, West-Estonian zone; IV, Tallinn zone; V, Alutaguse zone. Major faults: 1, Southern Finland shear zone; 2, Skonsero fault; 3, Paldisky–Pskov deformation zone; 4, Middle Estonian fault zone; 5, Tapa fault zone; 6, Koporsky fault; 7,  North Latvian fault zone; 8, deformations within the Vyborg rapakivi intrusions. The position of the rapakivi intrusions and rapakivi-like granites is shown in gray. Thin black dashed line denotes the boundary of the Shield. Blue line shows the northern boundary of the Baltic syncline.

 
Citation: Assinovskaya B. A., M. K. Ovsov (2014), Seismotectonic zoning of the Finnish–Bothnia region based on the structural analysis method, Russ. J. Earth Sci., 14, ES2005, doi:10.2205/2014ES000542.
 

Copyright 2014 by the Geophysical Center RAS.

Generated from LaTeX source by SemTeXML, v.1.2 software package.