Abstract
The mechanism of the earthquake focus is one of the most important parameters characterizing the seismic event. In modern seismology, it is associated with the sudden movement of rocks accompanied by the emission of seismic waves along the surface of weakened strength, and reflects simultaneously the spatial orientation of the axes of the principal stresses, possible planes of discontinuities and motions in the earthquake source, and represent almost the bulk of information on the stress state of the earth’s interior (Kangarli et al. 2017). It is data on the stress and strain fields, together with the geological, structural-tectonic structure, that make it possible to solve the problem of creating models of deformation processes in the tectonic structures of the earth’s crust (Sychev 2005).
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