Неплейттектоническое (автономное) складко- и надвигообразование в земной коре

Geophysical monitoring of the geological environment is one of the main directions in the geodynamic research which makes it possible to follow the processes in the Earth Crust. For prediction purposes it is interesting to know the statistics of the distribution of electromagnetic radiation anomalies which manifests itself in the marked periods of seismic processes. The task is to divide the sources of electromagnetic radiation into exogenous, endogenous and of anthropogenic origin. The law-based change in the distribution statistics of electromagnetic anomalies may be the result of the superposition of two processes. The total signal contains the effect from the close and far away earthquakes due to the wake-up of surface structures in the zones of dynamic influences of activated fissures and also radiation from anthropogenic seismicity which leads to the temporary surface breakup of blocks and, as a consequence, to the decrease of electromagnetic radiation.