Autosoliton View of the Seismic Process. Part 2. Possibility of Generation and Propagation of Slow Deformation Autosoliton Disturbances in Geomedia
2021
In the autosoliton view, the complete mathematical model of the seismic
process taken as the deformation and fracture process of a loaded geomedium
combines dynamic equations of solid mechanics and specific constitutive
equations for geomedium rheology. These equations describe both the conventional
stress-strain evolution due to the stress wave propagation with sound
velocities, which are governed by special features of constitutive equations,
and slow dynamics of the loaded strong medium. Numerical investigation is given
to the generation of deformation autosolitons, front structure, and propagation
of intra- and interfault deformation disturbances. Slow deformation disturbances
in real geomedium elements are numerically modeled.
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