The influence of crystallographic orientation and grain boundary migration on microstructural and textural evolution in an S-C mylonite
- 9 April 1987
- journal article
- Published by Elsevier in Tectonophysics
- Vol. 135 (1-3) , 155-169
- https://doi.org/10.1016/0040-1951(87)90158-2
Abstract
No abstract availableKeywords
This publication has 23 references indexed in Scilit:
- Fabric development in shear zones: theoretical controls and observed phenomenaPublished by Elsevier ,2003
- The partitioning of deformation in flowing rock massesPublished 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
- Kinematic and tectonic significance of microstructures and crystallographic fabrics within quartz mylonites from the Assynt and Eriboll regions of the Moine thrust zone, NW ScotlandEarth and Environmental Science Transactions of the Royal Society of Edinburgh, 1986
- Relationships between strain and quartz crystallographic fabrics in the Roche Maurice quartzites of Plougastel, western BrittanyJournal of Structural Geology, 1986
- S-C MylonitesJournal of Structural Geology, 1984
- Flow stress from microstructures of mylonites: Example and current assessmentJournal of Geophysical Research, 1980
- Dynamic recrystallization during creep of single‐crystalline halite: An experimental studyJournal of Geophysical Research, 1979
- Discussion: Crossed-girdle c-axis fabrics in quartzites plastically deformed by plane strain and progressive simple shearTectonophysics, 1977