Fig. 5From: Magnetotelluric characterization of the Alhama de Murcia Fault (Eastern Betics, Spain) and study of magnetotelluric interstation impedance inversionFrom top to bottom: plan views at two different depths, cross section beneath the profile and measured and predicted responses at Site 4 corresponding to the models obtained by inverting the synthetic data from Model 2: a impedance Z (left); b1 interstation impedance ZI (E:4;B:6) (middle) and, b2 quasi-impedance qZ (E:4;B:6) (right)Back to article page