Abstract
The electromagnetic radiation mechanisms guiding the seismic activity in closed regions are modelled as suitable network of cavities and waveguides connected with natural boundary layers, physically [1]-[6]. The non-smooth, non-uniform, and sharp changes of electric charges have stochastic influences on seismic activity. The spatial and temporal characteristics of these influences create the equivalent seismoelectromagnetic source of the activity. These equivalent seismo-electromagnetic sources threshold a suitable mechanism, which trigger the earthquake zones.
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