Fig. 25From: The effect of initial and prior models on phase tensor inversion of distorted magnetotelluric dataNS cross sections at the easting of 200 m of the models inverted from the synthetic model (Fig. 1) with near-surface distorters (Fig. 20) using different data types in the inversion, a PTATAN, b ZLOGO, and c ZLOGA, and using SSQ1D as the initial model (Fig. 24)Back to article page