Theory of compaction bands in porous rock

Physics and Chemistry of the Earth, Part A: Solid Earth and Geodesy

Volumn 26, Issue 1-2, 2001, Pages 95-100

  Issen, K A ^a   Rudnicki, J W ^a  

^a Northwestern University   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

COMPACTION; COMPRESSION; POROUS MEDIUM;

EID: 0035094696     PISSN: 14641895     EISSN: None     Source Type: Journal    
DOI: 10.1016/S1464-1895(01)00031-X     Document Type: Article

References (22)

1. Analysis of faulting in porous sandstones
2. Compacting and dilating shear bands in porous rock: Theoretical and experimental conditions
3. The initiation and propagation of dilatant rupture zones in geological materials
4. Material model for granular soils
5. Cap plasticity models and compactive and dilatant pre-failure deformation
6. Acceleration waves in solids
7. On constitutive inequalities for simple materials - I
8. Inelastic constitutive properties and shear localization in Tennessee marble
9. Conditions for compaction bands in porous rock
10. Conditions de stabilté et postulat de Drucker
11. Micromechanics of brittle faulting and cataclastic flow in Berea sandstone
12. Compaction bands: A structural analog for anti-mode I cracks in aeloian sandstone
13. Theoretical and experimental investigation of compaction bands
14. Rudnicki and Rice's analysis of strain localization revisited
15. Conditions for the localization of deformation in pressure-sensitive dilatant materials
16. Reexamination of fault angles predicted by shear localization theory
17. Effect of loading path and porosity on the failure mode of porous rocks
18. The transition from brittle faulting to cataclastic flow in porous sandstones: Mechanical deformation
19. Micromechanics of pressure-induced grain crushing in porous rock