To theory of seismic and electromagnetic monitoring of the modern geodynamic processes

Abstract

The spread-spectrum signals of endogenous nature observed during the field geophysical research are certain physical phenomena (Sobolev, 1993) that require appropriate theoretical description. The usage of these phenomena in a geophysical research is complicated by a lack of a phenomenological theory. At present certain approaches in creating of the theory are based on certain summaries of the well studied controlled sources. This makes it impossible either to predict properties of the observed signals or to explain them. The main task is to find the very transformation of the acoustic and electromagnetic emissions that would allow enunciating an inverse problem on the detection of the location of the field generation and activity of their sources.