Asymmetric shape preferred orientations as shear-sense indicators
- 1 April 1995
- journal article
- Published by Elsevier in Journal of Structural Geology
- Vol. 17 (4) , 509-517
- https://doi.org/10.1016/0191-8141(94)00080-j
Abstract
No abstract availableKeywords
This publication has 23 references indexed in Scilit:
- Orthogneiss, mylonite and non coaxial deformation of granites: the example of the South Armorican Shear ZonePublished by Elsevier ,2003
- Crack-seal fibre growth mechanisms and their significance in the development of oriented layer silicate microstructuresPublished by Elsevier ,2003
- Microstructures and c-axis fabrics indicative of quartz dissolution in sheared quartzites and phyllonitesPublished by Elsevier ,2003
- Coupled grain-scale dilatancy and mass transfer during deformation at high fluid pressures: examples from Mount Lyell, TasmaniaPublished by Elsevier ,2003
- The origin of laminated and massive anorthosite, Sept Iles layered intrusion, Québec, CanadaContributions to Mineralogy and Petrology, 1991
- Preferred Mineral Orientations Related to Magmatic Flow in Ophiolite Layered GabbrosJournal of Petrology, 1989
- Preferred orientation developed by rigid markers in two-dimensional simple shear strain: a theoretical and experimental studyTectonophysics, 1987
- Theoretical and experimental study of fabrics developed by different shaped markers in two-dimensional simple shearBSGF - Earth Sciences Bulletin, 1983
- Sense of nappe emplacement from quartz c-axis fabrics; an example from the Betic Cordilleras (Spain)Earth and Planetary Science Letters, 1982
- Un nouveau critere de sens de mise en place dans une caisse filonienne: Le “pincement” des mineraux aux epontesTectonophysics, 1979