Subbotin Institute of Geophysics of the NAS of Ukraine
Abstract
Identification of the nature of weak seismic events recorded in the East European Platform is based on the use of the analysis results for recording forms and spectral time diagrams. The difference between waveforms and spectral time diagrams of the local earthquakes (tectonic and technogeneous) and powerful industrial explosions has been noted. The relation between the sources of low-intensity seismic manifestations of tectonic origin and fractured zones in the Earth's crust has been determined
