and Dielectric Effects in Polymer Solids, Wiley, London (1967).
Seismic wave propagation in the earth has been known to be anelastic
due to the conversion of elastic energy into heat.
2012), the Boussinesq approximation was replaced by an anelastic
approximation to account for density variations in the vertical direction, and a simple, single-moment ice microphysics scheme is employed.
Seismic Wave Propagation in Laterally Heterogeneous Anelastic
Media: Theory and Applications to the Seismic Zonation.
as a guest researcher for fourteen months from July in 1997, where he studied on elastic and anelastic
properties of materials.
The equation of motion for incompressible flow may be generalized to atmospheric flows by the use of the so-called anelastic
The ASR (short for anelastic
strain recovery) technique is widely used in deep 3-D stress measurements of rocks in crustal drilling, especially in seismic fracture zones with complex geologic conditions and broken formations.
by elastic and anelastic
collisions, through an appropriate size of the energy range [DELTA][epsilon].
Some topics include: continental and oceanic lithosphere structure from long-range seismic profiling, the fate of subducted oceanic crust and the origin of intraplate volcanism, volatiles in the mantle lithosphere, deformable lithospheric plates, space and time variations of elastic and anelastic
properties in the shallow lithosphere, and possible paleoshorelines and the evolution of the lithosphere on Mars.
attenuation along the propagation path was parameterized using an attenuation value of [t.
The second application uses the modified Hart's model  to model elastic, plastic, anelastic
, micro-plastic and micro-anelastic
strain and their effects on the permanent deformation of bent beams .
The spectrum was not corrected for the effect of the anelastic
attenuation because this parameter is only important for frequencies f [much greater than] [f.