Laboratory measurement of seismic wave dispersion and attenuation at high pressure and temperature
At 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 d
|Collections||ANU Research Publications|
|Book Title:||Advances in High-pressure Technology for Geophysical Applications|
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