A general framework for the occurrence and faulting of deformation bands in porous granular rocks
Deformation bands form in porous granular rocks by localized inelastic yielding that is well described by a modified Cam cap model. All five kinematic varieties of bands observed in the field, including dilation bands, dilation bands with shear, shear bands, compaction bands with shear, and compacti...
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Veröffentlicht in: | Tectonophysics 2005-12, Vol.411 (1), p.1-18 |
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Format: | Artikel |
Sprache: | eng |
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