Influence of driving stress on cataclastic deformation and permeability in well cemented sandstones

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

Volumn 26, Issue 1-2, 2001, Pages 39-43

  Hutcheon, R ^a   Somerville, J ^a   Smart, B ^a  

^a HERIOT WATT UNIVERSITY   (United Kingdom)

Author keywords

[No Author keywords available]

Indexed keywords

FAULT GOUGE; MICROSTRUCTURE; PERMEABILITY; STRESS ANALYSIS;

EID: 0035097664     PISSN: 14641895     EISSN: None     Source Type: Journal    
DOI: 10.1016/S1464-1895(01)00020-5     Document Type: Article

References (13)

1. Effect of faulting on fluid flow in porous sandstones: Petrophysical properties
2. Implications for mechanical properties of brittle faults from observations of the punchbowl fault zone, CA
3. Fault tip displacement gradients and process zone dimensions
4. Experimental fault sealing: Shear band permeability dependency on cataclastic fault gouge characteristics
5. In-situ stress, pore pressure, and hydrocarbon migration and accumulation in sedimentary basins
6. Bracos river bar: A study in the significance of grain size parameters
7. Estimation of the effects of sub-seismic sealing faults on effective permeabilities in sandstone reservoirs
8. Deformation microstructures and diagenesis in sandstone adjacent to an extensional fault: Implications for the flow and entrapment of hydrocarbons
9. Crushing of single irregularly shaped particles by compression: Size distribution of progency particles
10. Permian and Triassic
11. Estimation of single-phase permeability from parameters of particle-size distribution
12. Geometry and development of relay ramps in normal fault systems
13. Micromechanics of pressure-induced grain crushing in porous rocks