The influence of surface conductive inhomogeneities on MT and MV soundings are analyzed by results of the physical modeling of geoelectromagnetic field of the Antarctic region. The 1D and 2D MT inversion results are compared.
Perspectives of the creating of the new physical models concerning the structure of the Earth, their evolution and methodology of the structure classification and parameter measuring of the Earth’s physical fields are analyzed. It is pointed out that investigation of the deep structure, composition and geodynamics of the continental and oceanic lithosphere gives the possibility to distinguish the system connected with global processes of Earth’s development (rifts, uncompensated deeps, continents, oceans).