Abstract
Five new heat flow values obtained in deep boreholes in the Western Carpathians are presented. Three holes were located in pre-Neogene folded units, the other two holes in Tertiary volcanites. The heat flow values range from 50.7 to 73.3 mW m −2 with an average value of 65.9 mW m −2 and they represent very needed information on the geothermal field in an area where heat flow values are still scarce.
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