Kinematics of orogenic collapse in the Variscan Pyrenees deduced from microstructures in porphyroblastic rocks from the Lys-Caillaouas massif
- 1 November 1994
- journal article
- Published by Elsevier in Tectonophysics
- Vol. 238 (1-4) , 139-160
- https://doi.org/10.1016/0040-1951(94)90053-1
Abstract
No abstract availableThis publication has 32 references indexed in Scilit:
- Foliation-boudinage control on the formation of the Rosebery PbZn orebody, TasmaniaPublished by Elsevier ,2003
- Foliation development — The contribution, geometry and significance of progressive, bulk, inhomogeneous shorteningPublished by Elsevier ,2003
- Collapse of the thickened Variscan crust in the French Massif Central: Mont Pilat extensional shear zone and St. Etienne Late Carboniferous basinPublished by Elsevier ,2003
- Extensional tectonics, basement uplift and Stephano-Permian collapse basin in a late Variscan metamorphic core complex (Montagne Noire, Southern Massif Central)Published by Elsevier ,2003
- Porphyroblast non-rotation during crustal extension in the Variscan Lys-Caillaouas Massif, PyreneesJournal of Structural Geology, 1995
- Step-wise growth of biotite porphyroblasts in pelitic schists of the western Lys-Caillaouas massif (Pyrenees)Journal of Structural Geology, 1986
- The geological significance of the western termination of the Mérens Fault at Port Vell (central Pyrenees)Tectonophysics, 1986
- A rifted tectonic setting for hercynian high-thermal gradient metamorphism in the pyreneesTectonophysics, 1986
- The variscan geology of the PyreneesTectonophysics, 1986
- Characteristics and mode of emplacement of gneiss domes and plutonic domes in central-eastern PyreneesJournal of Structural Geology, 1982