“…At variance with the fluid case, elastic materials are generically anisotropic and, in addition to the usual longitudinal matter perturbations, there exist also transverse perturbations. We denote the speeds of longitudinal and transverse perturbations along the radial (tangential) direction as c L (δ, η) and c T (δ, η) (c L (δ, η) and cT (δ, η)), respectively [6,7].…”