Jackson, Ian2015-12-100444519289http://hdl.handle.net/1885/39118At high temperature and long periods, and in the presence of fluids, viscoelastic relaxation can lead to substantial departures from the ideal elastic behavior of geological materials. The nonelastic behavior is associated with the stress-induced perturbaKeywords: Anelasticity; Dislocation damping; Grain-boundary sliding; Partial melting; Phase transformations; Seismic wave attenuation; Seismic wave dispersion; ViscoelasticityProperties of Rock and Minerals - Physical Origins of Anelasticity and Attenuation in Rock200710.1016/B978-044452748-6.00046-82016-02-24