The economic use of deep geothermal energy is fundamentally controlled by the factors of rock permeability, temperature gradient, and depth. The carbonates of the Northern Limestone Alps are considered possible hydrothermal deep aquifers in Tyrol. This is the so-called main dolomite and Wetterstein limestone. For an initial assessment of the geothermal potential, information from the deep Kramsach Th1 borehole was used. With a...