Chapter 5 Localization: Shear bands and compaction bands
Abstract
The localized deformation is a ubiquitous phenomenon in geomaterials. It occurs over a vast range of size scales, from the microscale level of grains to faults extending over hundreds of kilometers. It occurs in a variety of forms: a concentration or coalescence of cracks; a distinct, planar frictional surface; a gouge zone of finely comminuted material; or simply a region of higher shear strain. In geomaterials, the severe shearing in regions...
Paper Details
Title
Chapter 5 Localization: Shear bands and compaction bands
Published Date
Jan 1, 2004
Journal
Volume
89
Pages
219 - 321
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