Inversion Strategy - Models and Methods of Magnetotellurics - page 482

⊥ from the TS-4 and TS models

Fig. 12.25 Comparison of impedance apparent resistivities

backgrounds is that in the case of the symmetric background the horizontal changes
of resistivity in the upper crust and crustal conductive layer are less strong.
In closing, we turn back to the starting model with asymmetrical normal back-
ground and perform the parallel inversion of all response functions (Re W zy ,Im W zy ,

Fig. 12.26 Averaging the
longitudinal apparent-
resistivty curves obtained

at the edges of profile