Quartz deformation in a very fine grained quartzo-feldspathic mylonite: a lack of evidence for dominant grain boundary sliding deformation
- 27 December 1999
- journal article
- Published by Elsevier
- Vol. 17 (8) , 1095-1109
- https://doi.org/10.1016/0191-8141(95)00007-z
Abstract
No abstract availableKeywords
This publication has 62 references indexed in Scilit:
- Dislocation creep regimes in quartz aggregatesPublished by Elsevier ,2003
- Preferred crystallographic orientation development during the plastic and superplastic flow of calcite rocksPublished by Elsevier ,2003
- Strain path partitioning within thrust sheets: microstructural and petrofabric evidence from the Moine Thrust zone at Loch Eriboll, northwest ScotlandPublished by Elsevier ,2003
- Microstructural shear criteria associated with grain-boundary sliding during ductile deformationPublished by Elsevier ,2003
- On mylonites in ductile shear zonesPublished by Elsevier ,2003
- Dynamic recrystallization of quartz under greenschist conditionsJournal of Structural Geology, 1994
- Microstructural and crystal fabric evolution during shear zone formationJournal of Structural Geology, 1992
- Grain size distribution and flow stress in tectonitesJournal of Structural Geology, 1984
- Grain-size sensitive deformation of a stretched conglomerate from Plymouth, VermontJournal of Structural Geology, 1980
- Fault rocks as indicators of progressive shear deformation in the Guingamp region, BrittanyJournal of Structural Geology, 1979