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Transient creep and strain energy dissipation: An experimental perspective

Faul, Ulrich; Jackson, Ian

Description

Energy dissipation due to intrinsic attenuation occurs at elevated temperatures in rocks as a result of a range of processes. Examples where small-strain, transient deformation occurs are seismic waves, tidal deformation, and at longer timescales post-glacial rebound and far-field post-seismic deformation. Experiments at mantle temperatures and seismic frequencies show that grain boundary sliding is a key process that results in a broad absorption band, as indicated by seismic observations....[Show more]

CollectionsANU Research Publications
Date published: 2015
Type: Journal article
URI: http://hdl.handle.net/1885/69957
Source: Annual Review of Earth and Planetary Sciences
DOI: 10.1146/annurev-earth-060313-054732

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