Collapse of the thickened Variscan crust in the French Massif Central: Mont Pilat extensional shear zone and St. Etienne Late Carboniferous basin
- 27 March 2003
- journal article
- Published by Elsevier
- Vol. 177 (1-3) , 139-149
- https://doi.org/10.1016/0040-1951(90)90278-g
Abstract
No abstract availableKeywords
This publication has 47 references indexed in Scilit:
- Orthogneiss, mylonite and non coaxial deformation of granites: the example of the South Armorican Shear ZonePublished by Elsevier ,2003
- Computer models of pressure shadows: a method for strain measurement and shear-sense determinationPublished by Elsevier ,2003
- Criteria for the sense of movement on fault surfaces in brittle rocksPublished by Elsevier ,2003
- Large-scale foliation boudinage in gneissesJournal of Structural Geology, 1988
- Shear criteria in rocks: an introductory reviewJournal of Structural Geology, 1987
- A 3-D kinematic model of fabric development in polycrystalline aggregates: comparisons with experimental and natural examplesJournal of Structural Geology, 1987
- Rolling structures at large shear strainJournal of Structural Geology, 1987
- Kinematics of compressional and extensional ductile shearing deformation in a metamorphic core complex of the northeastern basin and rangeJournal of Structural Geology, 1987
- Geochemical comparison between Himalayan and Hercynian leucogranitesPhysics of the Earth and Planetary Interiors, 1984
- Role of tectonic denudation in warping and uplift of low-angle normal faultsGeology, 1984