Abstract
Results of magnetotelluric soundings have been obtained for a series of five field stations located approximately along the international profile of deep seismic sounding No. VI. Multilayer sounding curves at almost all stations show anisotropic and/or horizontally non-homogeneous situation. Methods for estimating the inhomogeneity measures were applied and attempts have been made to locate the homogeneity axis and corresponding two-dimensional structures. Directional properties of the electric conductivity have been discussed and fitted to the local geology.
On respecting the uncertainty and ambiguity of apparent resistivity curves the depths of remarkable discontinuities have been estimated and traced along the profile.
