Experimental investigation into the microstructural and mechanical evolution of phyllosilicate-bearing fault rock under conditions favouring pressure solution
- 21 June 2001
- journal article
- Published by Elsevier
- Vol. 23 (8) , 1187-1202
- https://doi.org/10.1016/s0191-8141(00)00184-x
Abstract
No abstract availableKeywords
This publication has 38 references indexed in Scilit:
- Strength and anisotropy of foliated rocks with varied mica contentsPublished by Elsevier ,2003
- The origin of S-C mylonites and a new fault-zone modelPublished by Elsevier ,2003
- Extensional structures in anisotropic rocksPublished by Elsevier ,2003
- On mylonites in ductile shear zonesPublished by Elsevier ,2003
- 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
- The strength profile for bimineralic shear zones: an insight from high-temperature shearing experiments on calcite–halite mixturesTectonophysics, 1998
- A theory for granular flow accommodated by material transfer via an intergranular fluidTectonophysics, 1995
- Experimental deformation of muscoviteJournal of Structural Geology, 1993
- Frictional dependence of gouge mixtures of quartz and montmorillonite on velocity, composition and fabricTectonophysics, 1987
- Secondary cleavages in ductile shear zonesJournal of Structural Geology, 1984