Fig. 4From: Magnetotelluric characterization of the Alhama de Murcia Fault (Eastern Betics, Spain) and study of magnetotelluric interstation impedance inversionLeft: plan view at the surface (top) and cross section beneath the profile (bottom) for synthetic Model 2. Right: responses calculated at Site 4 from Z (dots) and ZI (lines): xy and yx components (top) and xx and yy components (bottom)Back to article page