RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 20, ES6014, doi:10.2205/2020ES000752, 2020

Figure 1. Geological map of the Nizne-Kansk massif. 1 - boundaries: established (a), assumed (b), unconformity (c), dropping (d); 2 - reverse faults: major (a), minor (b), faults (c); 3 - breaking faults: unidentified (a), alleged (b), activated (c); 4 - mylonites (a), blastomylonites (c); 5 - tectonic terrain ledges; 6 - amphibolites (a), shales (b); 7 - migmatites (a), granitoids (b); 8 - diaftorites; 9 - outcrops; 10 - places of permafrost; 11 - holes; 12 - wells in area HLRW; 13 - thickness of the Quaternary layer; 14 - the relationship of layers: consonant (a), unconformable (b), angular unconformity (c), tectonic (d), intrusive (e); 15 - boundaries of areas for HLRW.

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Citation: Agayan S. M., V. N. Tatarinov, A. D. Gvishiani, Sh. R. Bogoutdinov, I. O. Belov (2020), FDPS algorithm in stability assessment of the Earth's crust structural tectonic blocks, Russ. J. Earth Sci., 20, ES6014, doi:10.2205/2020ES000752.
 

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