Sense of shear in high-temperature movement zones from the fabric asymmetry of plagioclase feldspars
- 1 January 1988
- journal article
- Published by Elsevier in Journal of Structural Geology
- Vol. 10 (1) , 73-81
- https://doi.org/10.1016/0191-8141(88)90129-0
Abstract
No abstract availableKeywords
This publication has 25 references indexed in Scilit:
- Fabric transitions in the Saxony granulite terrainPublished by Elsevier ,2003
- C-slip in quartz from subsolidus deformed granitePublished by Elsevier ,2003
- The Himalayan Main Central Thrust pile and its quartz-rich tectonites in central NepalPublished by Elsevier ,2003
- Preferred orientation of plagioclase—neutron diffraction and U-stage dataTectonophysics, 1986
- High-temperature emplacement of the Los Reales peridotite nappe (Betic Cordillera, Spain)Journal of Structural Geology, 1986
- Two distinct late Precambrian (Avalonian) terranes in southeastern New England and their late Paleozoic juxtapositionAmerican Journal of Science, 1985
- Plagioclase microfabrics in a ductile shear zone from the Jotun Nappe, NorwayJournal of Structural Geology, 1985
- Petrofabric analysis of Saxony Granulites by optical and X-ray diffraction methodsTectonophysics, 1979
- Plastic deformation of quartzites at low temperature in an area of natural strain gradientTectonophysics, 1977
- Plastic-deformati on mechanisms in quartz: The effect of waterTectonophysics, 1975