Microstructure of deformed biotite defining foliation in cataclasite zones in granite, central Japan
- 1 January 1991
- journal article
- Published by Elsevier in Journal of Structural Geology
- Vol. 13 (7) , 777-785
- https://doi.org/10.1016/0191-8141(91)90003-2
Abstract
No abstract availableKeywords
This publication has 34 references indexed in Scilit:
- Orthogneiss, mylonite and non coaxial deformation of granites: the example of the South Armorican Shear ZonePublished by Elsevier ,2003
- Shear criteria in granite and migmatite deformed in the magmatic and solid statesPublished by Elsevier ,2003
- Strain pattern in the Aar Granite (Central Alps): Orthogneiss developed by bulk inhomogeneous flatteningPublished by Elsevier ,2003
- Origin of kinkbands and shear-band cleavage in shear zones: an experimental studyJournal of Structural Geology, 1990
- Factors affecting the kinematic interpretation of asymmetric boudinage in shear zonesJournal of Structural Geology, 1988
- Deformation mechanisms in granitic rocks at shallow crustal levelsJournal of Structural Geology, 1988
- The use of asymmetric pressure shadows in mylonites to determine the sense of shearJournal of Structural Geology, 1988
- Composite planar fabric of gouge from the Punchbowl Fault, CaliforniaJournal of Structural Geology, 1987
- Deformation of granitic rocks across the brittle-ductile transitionJournal of Structural Geology, 1985
- Brittle to ductile transition due to large strains along the White Rock thrust, Wind River mountains, WyomingJournal of Structural Geology, 1984