On the internal structure and mechanics of large strike-slip fault zones: field observations of the Carboneras fault in southeastern SpainD. R. Faulkner, E. H. Rutter, Alastair C. Lewis|Tectonophysics|2003Cited by 541
Strength, porosity, and permeability development during hydrostatic and shear loading of synthetic quartz‐clay fault gougeBrian Crawford, E. H. Rutter, D. R. Faulkner|Journal of Geophysical Research Atmospheres|2008Cited by 275
Can the maintenance of overpressured fluids in large strike-slip fault zones explain their apparent weakness?D. R. Faulkner, E. H. Rutter|Geology|2001Cited by 257
Comparisons of water and argon permeability in natural clay‐bearing fault gouge under high pressure at 20°CD. R. Faulkner, E. H. Rutter|Journal of Geophysical Research Atmospheres|2000Cited by 206
The gas permeability of clay-bearing fault gouge at 20°CD. R. Faulkner, E. H. Rutter|Geological Society London Special Publications|1998Cited by 106