Fig. 13From: Porosity–permeability relationship derived from Upper Jurassic carbonate rock cores to assess the regional hydraulic matrix properties of the Malm reservoir in the South German Molasse BasinDistribution of permeability measured on rock cores compared to permeability modeled by the GPPT. a Distribution within the stratigraphic units of the Malm reservoir. b Dependence of permeability on particle and crystal size as well as on the morphology of dolomite crystals (c)Back to article page