The present work focuses on the estimation of anisotropy and its influence on the interpretation. Anisotropy of the subsurface is estimated using the transition zone measurements of Controlled-Source Radiomagnetotellurics (CSRMT) field measurements. In addition, the electrical resistivity measurements were also conducted The CSRMT results are compared with the electrical resistivity tomography data. The results of our anisotropic inversions are in good agreement with the existing theory. This has been verified by ubstituting the resistivity values, obtained from the electromagnetic and direct current inversion, in the theoretical equations. Results of anisotropic inversions are well correlated with the borehole data, well logging data and a priori information about the geology of the study area.