Fig. 4From: Granitic and magmatic bodies in the deep crust of the Son Narmada Region, Central India: constraints from seismic, gravity and magnetotelluric methods(a) Apparent resistivity and phase data in the form of pseudo-sections for both the TM and TE modes along with the model (shown in Fig. 5(a)) response (b) Apparent resistivity, phase data, and model responses for a few stations. RMS errors are also shown. (c) Plot of sensitivity values for the model.Back to article page