How phyllosilicate mineral structure affects fault strength in Mg‐rich fault systemsC. Sanchez Roa, Fernando Nieto, Juan Jiménez‐Millán 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, Juan Jiménez‐Millán 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
Micromechanics of Friction in a Detailed Study of Mg-rich PhyllosilicatesC. Sanchez Roa, Fabiola Kessler Nieto, Carolyn Boulton et al.|AGUFM|2016Cited by 0