Fig. 1From: Intrinsic attenuation from inhomogeneous waves in a dissipative anisotropic poroelastic mediumVariations of phase velocity (υ) and homogeneous attenuation (β) and inhomogeneity strength (δ) of qP1-wave with propagation direction (θ) and quality factor (Q) in pre-stressed sandstone of triclinic anisotropy; ω = ωc.Back to article page