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Autosoliton View of the Seismic Process. Part 2. Possibility of Generation and Propagation of Slow Deformation Autosoliton Disturbances in Geomedia

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Abstract

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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  • 31 August 2021

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Funding

The work is performed at the support of the Russian Science Foundation (Project No. 19-17-00122).

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Authors and Affiliations

  1. National Research Tomsk State University, 634050, Tomsk, Russia

    P. V. Makarov, I. Yu. Smolin, M. O. Eremin, R. A. Bakeev, A. Yu. Peryshkin, V. A. Zimina, A. Chirkov, A. A. Kazakbaeva & A. Zh. Akhmetov

  2. Institute of Strength Physics and Materials Science, Siberian Branch, Russian Academy of Sciences, 634055, Tomsk, Russia

    P. V. Makarov, I. Yu. Smolin, Yu. A. Khon, M. O. Eremin, R. A. Bakeev, A. Yu. Peryshkin, V. A. Zimina & A. Zh. Akhmetov

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  1. P. V. Makarov
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  2. I. Yu. Smolin
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Correspondence to I. Yu. Smolin.

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Makarov, P.V., Smolin, I.Y., Khon, Y.A. et al. Autosoliton View of the Seismic Process. Part 2. Possibility of Generation and Propagation of Slow Deformation Autosoliton Disturbances in Geomedia. Phys Mesomech 24, 375–390 (2021). https://doi.org/10.1134/S1029959921040044

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