Jackson, Ian2015-12-132015-12-130444519793http://hdl.handle.net/1885/83837At sufficiently high temperatures and in the presence of fluids, the small-strain mechanical behavior of geological materials is inevitably frequency dependent. In order to understand the nature of viscoelastic relaxation manifest in the attenuation and dLaboratory measurement of seismic wave dispersion and attenuation at high pressure and temperature200510.1016/B978-044451979-5.50007-72015-12-12