Fig. 8From: The effect of initial and prior models on phase tensor inversion of distorted magnetotelluric dataNorth–south (NS) cross sections at the easting of 200 m of the models inverted from the undistorted data using (a, d, g, j) PTATAN, (b, e, h, k) ZLOGA, and (c, f, i, l) ZLOGO with different initial models. The geometry of anomalies in the input model (Fig. 1) is represented by the gray solid lineBack to article page