Original paper
Quasi-static fault growth and shear fracture energy in granite
Abstract
The failure process in a brittle granite sample can be stabilized by controlling axial stress to maintain a constant rate of acoustic emission. As a result, the post-failure stress curve can be followed quasi-statically, extending to hours the fault growth process which normally would occur violently in a fraction of a second. Using a procedure originally developed to locate earthquakes, acoustic emission arrival-time data are inverted to obtain...
Paper Details
Title
Quasi-static fault growth and shear fracture energy in granite
Published Date
Mar 1, 1991
Journal
Volume
350
Issue
6313
Pages
39 - 42
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Notes
History