oa Modeling of Stress-Strain State of Anisotropic Lithosphere Near the Earthquake Focus

References

1. Burov, E.B. (2010). The equivalent elastic thickness (T), seismicity and the long-term rheology of continental lithosphere: Time to burn out “crème brulee”. Insights from large-scale geodynamic modeling. Tectonophysics, 484, 4–26.
   [Google Scholar]
2. Karato, S. (2008). Deformation of Earth materials. An introduction to the rheology solid Earth.Cambridge University Press, Cambridge.
   [Google Scholar]
3. Karnauhov, V.G., Kirichok, I.F. (1986). Connected problems of viscoelastic plates and shells. Naukova dumka, Kiev. (in Russian).
   [Google Scholar]
4. Lubkov, M.V. (2011). Modeling of the strain-deformable state and anomalous gravity field in the epicenter of the earthquake. Geoіnformatika, 1, 51–56. (in Ukrainian).
   [Google Scholar]
5. Spirtus, V.B., Savchuk, E.V. (2006). Specific fiches of the creep and brittle damage at the shifting deformation of viscoelastic of defective environment. Geofiz. zhurn., 28(2), 123–129. (in Russian).
   [Google Scholar]
6. Tjorkot, D., Shubert, D. (1985). Geodynamics. Geological applications of the continuum physics.Mir, Moscow. (in Russian).
   [Google Scholar]
7. Sherman, S.I. (2005). Tectonophysical analysis of the seismic processes in the lithosphere active faults zones and problem of average daily earthquake forecast. Geofiz. zhurn., 27(1), 20–38. (in Russian).
   [Google Scholar]
8. Wright, T.J. (2016). The earthquake deformation cycle. Astronomy and Geophysics, 57, 4.20–4.26.
   [Google Scholar]