Figure 2From: Exploration for deep geothermal reservoirs in Luxembourg and the surroundings - perspectives of geothermal energy useGeological cross sections of the Trier-Luxembourg Embayment (modified from Schintgen and Förster 2013). For location, see Figure 1a. Vertical exaggeration is tenfold for profile B and 7.5-fold for profile C. Black dashed lines correspond to intersection with the indicated cross section.Back to article page