Mechanical compaction, microstructures and permeability evolution in sandstones

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

Volumn 26, Issue 1-2, 2001, Pages 45-51

  David, C ^a   Menendez, B ^a   Zhu, W ^b   Wong, T F ^c  

^a UNIVERSITÉ DE CERGY PONTOISE   (France)

^b WOODS HOLE OCEANOGRAPHIC INSTITUTION   (United States)

^c STONY BROOK UNIVERSITY   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

COMPACTION; MICROSTRUCTURE; PERMEABILITY; SANDSTONE;

EID: 0035091045     PISSN: 14641895     EISSN: None     Source Type: Journal    
DOI: 10.1016/S1464-1895(01)00021-7     Document Type: Article

References (20)

1. Microstructure of deformation bands in porous sandstones at Arches National Park, Utah
2. Small faults formed as deformation bands in sandstones
3. A note on permeability change in geological materials due to stress
4. Geometry of flow paths for fluid transport in rocks
5. Laboratory measurement of compaction-induced permeability change in porous rocks: Implications for the generation and maintenance of pore pressure excess in the crust
6. Fault sealing during deformation band growth in porous sandstone
7. Sequential growth of deformation bands in the laboratory
8. Micromechanics of brittle faulting and cataclastic flow in Berea sandstone
9. The pore geometries of reservoir rocks
10. The transition from brittle faulting to cataclastic flow: Mechanical deformation
11. Brittle faulting and permeability evolution: Hydromechanical measurement, microstructural observation, and network modeling
12. Micromechanics of pressure-induced grain crushing in porous rocks
13. Network modeling of permeability evolution during cementation and hot isostatic pressing 1995
14. Permeability reduction in a dilatant rock: Network modeling of damage and tortuosity
15. The transition from brittle faulting to cataclastic flow: Permeability evolution
16. Network modeling of the evolution of permeability and dilatancy in compact rock
17. Effect of high pressure deformation on permeability of Ottawa sand