Fig. 8From: Petrophysical properties of the Muschelkalk from the Soultz-sous-Forêts geothermal site (France), an important lithostratigraphic unit for geothermal exploitation in the Upper Rhine Grabena Representative dry stress–strain curves (box number indicated next to each curve), b dry uniaxial compressive strength as a function of connected porosity, and c dry Young’s modulus as a function of connected porosity for Muschelkalk samples from exploration well EPS-1 (Soultz-sous-Forêts)Back to article page