Fig. 1From: How temperatures derived from fluid flow and heat transport models impact predictions of deep geothermal potentials: the “heat in place” method applied to Hesse (Germany)a Position of the model area marked by a green contour; sediments of the European Cenozoic Rift System (ECRS) in yellow and of the North German Basin (NGB) in pale yellow; b topographic map of Hesse [modified after Koltzer et al. (2019a); topography: NOAA National Geophysical Data Center (2009)]. c Structural model of Hesse, the view is from southeast [modified after Arndt et al. (2011)]. The used graphics software was (Adobe Inc. 2019)Back to article page