Development of preferred orientation and microstructure in sheared quartzite: comparison of natural data and simulated results
- 1 November 1999
- journal article
- Published by Elsevier in Tectonophysics
- Vol. 312 (2-4) , 133-155
- https://doi.org/10.1016/s0040-1951(99)00173-0
Abstract
No abstract availableThis publication has 42 references indexed in Scilit:
- Fabric transitions in the Saxony granulite terrainPublished by Elsevier ,2003
- Fabric development in shear zones: theoretical controls and observed phenomenaPublished by Elsevier ,2003
- Dislocation creep regimes in quartz aggregatesPublished by Elsevier ,2003
- The simulation of fabric development during plastic deformation and its application to quartzite: the influence of deformation historyPublished 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
- Extensional structures in anisotropic rocksPublished by Elsevier ,2003
- The evolution of high-temperature mylonitic microfabrics: evidence from simple shearing of a quartz analogue (norcamphor)Journal of Structural Geology, 1996
- Dynamic recrystallization of quartz under greenschist conditionsJournal of Structural Geology, 1994
- SEM electron channelling analysis of dynamic recrystallization in a quartz grainJournal of Structural Geology, 1991
- Simulation of fabric development in recrystallizing aggregates—I. Description of the modelJournal of Structural Geology, 1988