Studies of geosolitons in the Crimean-Black Sea region in the models
of Fitz-Hew-Nagumo type
© Spirtus V.B.
The main features of migration of seismic activity in the Crimean-Black Sea region were explored. This feature - the splitting of seismicity into two branches: western and eastern one after the Crimean earthquake of 1927 (M>6,8) and inverse dependence of speed of migration of shocks on the power level of seismic events. It is shown that they can be interpreted within the framework of the known biophysical model of FHN type.