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Specific features of earthquake manifestation in seismotectonic deformation field
Author(s) -
Ольга Анатольевна Кучай
Publication year - 2010
Publication title -
geodinamika i tektonofizika
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.336
H-Index - 8
ISSN - 2078-502X
DOI - 10.5800/gt-2010-1-3-0022
Subject(s) - geology , seismology , deformation (meteorology) , field (mathematics) , stress field , boundary (topology) , geophysics , geodesy , physics , mathematical analysis , oceanography , mathematics , finite element method , pure mathematics , thermodynamics
Earthquake concentration areas in the changeable stress-strain medium are considered. In strong earthquake centres, rupturing occurs within the limits of the arbitrarily-set boundary between deformations of positive and negative values in the field of latitudinal, meridional and vertical components of seismotectonic deformation (Fig. 1–12)

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