Abstract
Abstract In eight areas of Central and Eastern Europe elevated electrical conductivity horizons determined from magnetotellurics, heat flow densities and crustal structure were identified. Based on these data, it was determined whether good conducting horizons are the consequence of elevated temperatures or not. In three areas investigated the thermal activation was detectable; these areas are Alpine subsidences. In the five other areas no thermal activation was found, the good conducting layers on these areas have been caused by other disturbing effects, such as material inhomogeneities or near surface disturbances.
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