Fig. 6From: Characterizing the physical properties of rocks from the Paleozoic to Permo-Triassic transition in the Upper Rhine GrabenP-wave velocity as a function of total porosity and permeability as a function of connected porosity for all rocks, organised by sample location. a Saint Pierre Bois. b Raon l’Etape. c Albersweiler. d WaldhambachBack to article page