Abstract
Publisher Summary This chapter focuses on the approaches for solving the forward and inverse problems. The chapter considers the methodological questions, the answers to which are wider than being case-descriptive only: These methodological questions are important not only for understanding the magnetotelluric (MT) field behavior as this applies to a specific given problem, but also for the effective interpretation of MT data in similar situations. Although electromagnetic data for the area in question are of an extremely nonsystematic nature, their analysis has revealed certain regularities in the behavior of the electric and magnetic fields, as well as Wiese vectors, which made it possible to put forward some hypotheses concerning the geoelectric structure of the region. To prove or disprove them, four alternative models of electric conductivity distribution in this region were constructed, which differ in the type of near-surface conductivity structure and in the presence or absence of a conducting channel linking the Black and Caspian seas. Among a wide range of experimental studies aimed at investigation of natural and artificially induced seismic, deformational and fluid-dynamical processes in a pay strata, and hosting rock and in the upper part of the section, a considerable part belongs to a complex of geophysical studies.
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