Relationships between pore space anisotropy and anisotropy of physical properties of silicoclastic rocks from the Corbières-Minervois fold-and-thrust-belt (north-east Pyrenees, France)

► Petrophysical anisotropies as reflecting petrofabric of weakly deformed sediments. ► Magnetic and electric anisotropy is controlled by the preferred orientation of phylosilicates. ► P-waves anisotropy is controlled by the orientation of porous space. ► The orientation of porous space is sensitive to the increase of layer parallel shortening (LPS). ► The void space is early controlled by deformation and is thus passively rotated during folding.