Pore Fluid Pressure Development in Compacting Fault Gouge in Theory, Experiments, and NatureD. R. Faulkner, Sabine A.M. den Hartog, C. Sanchez Roa et al.|Journal of Geophysical Research Solid Earth|2017Cited by 153
How phyllosilicate mineral structure affects fault strength in Mg‐rich fault systemsC. Sanchez Roa, Fernando Nieto, Carolyn Boulton et al.|Geophysical Research Letters|2017Cited by 29
Fibrous clay mineral authigenesis induced by fluid-rock interaction in the Galera fault zone (Betic Cordillera, SE Spain) and its influence on fault gouge frictional propertiesC. Sanchez Roa, Francisco Juan García-Tortosa, Fernando Nieto et al.|Applied Clay Science|2016Cited by 24
Micro- and nano-scale study of deformation induced mineral transformations in Mg-phyllosilicate-rich fault gouges from the Galera Fault Zone (Betic Cordillera, SE Spain)C. Sanchez Roa, D. R. Faulkner, Blanca Bauluz et al.|American Mineralogist|2018Cited by 9
Implications of sepiolite dehydration for earthquake nucleation in the Galera Fault Zone: A thermodynamic approachC. Sanchez Roa, D. R. Faulkner, Olivier Vidal et al.|Applied Geochemistry|2017Cited by 6