Viscoelastic relaxation in olivine: an experimental study of alternative mechanisms
Observation and analysis of seismic waves is the predominant mechanism in which geophysicists infer the structure and state of the Earth’s interior, including aspects such as major element composition, grain size, temperature, melt fraction and water content. However, imperative to this inversion, is obtaining a robust understanding of how changes in any of these specific physical characteristics manifest as seismic anomalies. In this thesis we conduct...[Show more]
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