Fig. 28
From: The effect of initial and prior models on phase tensor inversion of distorted magnetotelluric data
NS cross sections at the easting of 200 m of the models inverted from the synthetic model (Fig. 1) with near-surface distorters (Fig. 20). All used SSQ1D as the initial model, but the prior models, a UHS100 and b UHS1000, were examined. The result of SSQ1D/UHS10 is not shown, as its inversion did not converge