Preferred lattice orientations of plagioclase from amphibolite and greenschist facies rocks near the Insubric Line (Western Alps)
- 1 April 1987
- journal article
- Published by Elsevier in Tectonophysics
- Vol. 135 (1-3) , 233-242
- https://doi.org/10.1016/0040-1951(87)90164-8
Abstract
No abstract availableKeywords
This publication has 15 references indexed in Scilit:
- The kinematics of movements along the Insubric Line and the emplacement of the Ivrea ZoneTectonophysics, 1987
- Textures and c-axis orientations of deformed quartz crystals from porphyric dikes of the Alpine »Root Zone« (Western Alps)International Journal of Earth Sciences, 1986
- Natural deformation and recrystallization of some intermediate plagioclase feldsparsTectonophysics, 1985
- Plagioclase microfabrics in a ductile shear zone from the Jotun Nappe, NorwayJournal of Structural Geology, 1985
- Analysis of dislocations in some naturally deformed plagioclase feldsparsPhysics and Chemistry of Minerals, 1984
- Fabric and origin of gneissic layers in anorthositic rocks of the St. Charles sill, OntarioCanadian Journal of Earth Sciences, 1981
- The relation between microfabric and strain in a progressively deformed quartzite sequence from Central AustraliaTectonophysics, 1976
- Studies of Igneous and Tectonic Textures and Layering in the Rocks of the Gosse Pile Intrusion, Central AustraliaJournal of Petrology, 1973
- Mechanical twinning and slip in experimentally deformed plagioclasesContributions to Mineralogy and Petrology, 1969
- Regional Study of Epidote, Mica, and Albite Fabrics of the MoinesGeological Magazine, 1957