Abstract

At present, one of the effective methods in the study of the geoelectrical inhomogeneity is the magnetovariational one in which relations between the variable components Ho H, H, of the geomagnetic field are given by Wiese - Parkinson matrix. There are many modes of transforming and representing this matrix for obtaining the useful information (magnetic polarisation diagram, induction vector, magnetovariational vector, magnetovariational phase and ellipticity). We use the magnetovariational vector, magnetovariational phase and ellipticity here to study the geoelectrical inhomogeneities on two exemplar models.