Fig. 10From: Intrinsic attenuation from inhomogeneous waves in a dissipative anisotropic poroelastic mediumDirectional variations of radial distance for half-decay of particle motion with frame anelasticity (∈) for fixed (θ = 45°) propagation direction in pre-stressed sandstone of triclinic anisotropy; ω = 1000 sec-1.Back to article page