Effect of phyllosilicates on fluid-assisted healing of gouge-bearing faults
- 1 December 2000
- journal article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 184 (1) , 199-210
- https://doi.org/10.1016/s0012-821x(00)00304-6
Abstract
No abstract availableKeywords
This publication has 20 references indexed in Scilit:
- Frictional-viscous flow of simulated fault gouge caused by the combined effects of phyllosilicates and pressure solutionTectonophysics, 2000
- Slip behavior of simulated gouge‐bearing faults under conditions favoring pressure solutionJournal of Geophysical Research, 2000
- Deformation processes and weakening mechanisms within the frictional–viscous transition zone of major crustal-scale faults: insights from the Great Glen Fault Zone, ScotlandPublished by Elsevier ,2000
- Experimental Study of the Compaction of Phyllosilicate-Bearing Sand at Elevated Temperature and with Controlled Pore Water PressureJournal of Sedimentary Research, 2000
- Laboratory study of fault healing and lithification in simulated fault gouge under hydrothermal conditionsTectonophysics, 1997
- Rheology of the lithosphere in space and timeGeological Society, London, Special Publications, 1997
- Fault healing inferred from time dependent variations in source properties of repeating earthquakesGeophysical Research Letters, 1995
- Kinetics of pressure solution at halite‐silica interfaces and intergranular clay filmsJournal of Geophysical Research, 1995
- Scaling of the critical slip distance for seismic faulting with shear strain in fault zonesNature, 1993
- Friction of rocksPure and Applied Geophysics, 1978