Fault rock heterogeneity can produce fault weakness and reduce fault stabilityJohn Bedford, N. Lapusta, D. R. Faulkner|Nature Communications|2022Cited by 151
The stabilizing effect of high pore-fluid pressure along subduction megathrust faults: Evidence from friction experiments on accretionary sediments from the Nankai TroughJohn Bedford, Takehiro Hirose, D. R. Faulkner et al.|Earth and Planetary Science Letters|2021Cited by 75
The Role of Grain Size and Effective Normal Stress on Localization and the Frictional Stability of Simulated Quartz GougeJohn Bedford, D. R. Faulkner|Geophysical Research Letters|2021Cited by 64
Reaction fronts, permeability and fluid pressure development during dehydration reactionsHenri Leclère, John Wheeler, John Bedford et al.|Earth and Planetary Science Letters|2018Cited by 36
A 4D view on the evolution of metamorphic dehydration reactionsJohn Bedford, D. R. Faulkner, John Wheeler et al.|Scientific Reports|2017Cited by 33