Fig. 12From: Hybrid finite difference–finite element method to incorporate topography and bathymetry for two-dimensional magnetotelluric modelingThe apparent resistivities computed at \(T=1\,\hbox {s}\) of the bathymetric model for the E- and H- polarizations are shown at the left and right top, respectively, whereas those computed at \(T=10\,\hbox {s}\) are shown at the left and right bottom, respectivelyBack to article page