Combined thrusting and wrenching in the Ibero-Armorican arc: A corner effect during continental collision
- 23 October 2002
- journal article
- Published by Elsevier
- Vol. 61 (2) , 319-332
- https://doi.org/10.1016/0012-821x(82)90063-2
Abstract
No abstract availableKeywords
This publication has 22 references indexed in Scilit:
- Orthogneiss, mylonite and non coaxial deformation of granites: the example of the South Armorican Shear ZonePublished by Elsevier ,2003
- Variscan intracontinental deformation: The Coimbra—Cordoba shear zone (SW Iberian Peninsula)Published by Elsevier ,2003
- Strain patterns of pluton emplacement in a crust undergoing non-coaxial deformation, Sierra Morena, Southern SpainPublished by Elsevier ,2003
- The Southern part of the Armorican orogeny: A result of crustal shortening related to reactivation of a pre-Hercynian mafic belt during Carboniferous timeTectonophysics, 1982
- Mathematical removal of regional ductile strains in Central Brittany: Evidence for wrench tectonicsTectonophysics, 1982
- Is the Hercynien belt of Brittany a major shear zone?Nature, 1980
- Development of sheath folds in shear regimesJournal of Structural Geology, 1980
- Shear zones in the iberian arcJournal of Structural Geology, 1980
- Description and origin of banded deformation structures. II. Rheology and the growth of banded perturbationsCanadian Journal of Earth Sciences, 1977
- Slip-line field theory and large-scale continental tectonicsNature, 1976