Abstract
It is known from earlier MT soundings that at the southern boundary of the TCA, north of the Lake Balaton, the MT sounding curves strongly differ from the ID ones (opposite tendencies in TE and TM modes, overshooting in TM mode, etc.). It has also been experienced that the directional characteristics of the impedance polar diagrams can be followed over a large area, i.e. they represent a remote effect or structural MT anisotropy.
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