Abstract
The East Slovak Basin Area is from genetic viewpoint area which represents longitudinal intramount depression filled by Neogene sediments and volcanics. This basin morphologically represents north-eastern promontory of Pannonian Basins System. During more than 50 years of systematic oil-geological exploration a quantity of knowledge was gathered here, as on geological structure and hydrocarbon fields as on thermal setting and geothermal waters. It is a case of nearly 20 000 analysed water samples and temperature measurements in the depth span from surface up to 4200m what enables us to distinguish in this region several prospective geothermal areas.
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