Crustal-scale strain partitioning: footwall deformation below the Alpine Oligo-Miocene detachment of Corsica
- 1 January 1996
- journal article
- Published by Elsevier in Journal of Structural Geology
- Vol. 18 (1) , 41-59
- https://doi.org/10.1016/0191-8141(95)00075-o
Abstract
No abstract availableKeywords
This publication has 42 references indexed in Scilit:
- Transverse lineation and large-scale structures related to Alpine obduction in CorsicaPublished by Elsevier ,2003
- Orthogneiss, mylonite and non coaxial deformation of granites: the example of the South Armorican Shear ZonePublished by Elsevier ,2003
- Age of emplacement of the schistes lustres nappe, Alpine CorsicaPublished by Elsevier ,2003
- Extensional structures in anisotropic rocksPublished by Elsevier ,2003
- Structures and tectonic evolution of the external zone of Alpine CorsicaJournal of Structural Geology, 1992
- Isostatic rebound due to tectonic denudation: A viscous flow model of a layered lithosphereTectonics, 1992
- Uplift of deep crust during orogenic extensional collapse: A model based on field studies in the Sogn‐Sunnfjord Region of western NorwayTectonics, 1990
- Tertiary extension and contraction of lower‐plate rocks in the Central Mojave Metamorphic Core Complex, southern CaliforniaTectonics, 1990
- High-pressure-low-temperature metamorphism and polyphase alpine deformation at Sant'Andrea di cotone (eastern corsica, france)Tectonophysics, 1981
- Reorientation of inclusions by combination of pure shear and simple shearTectonophysics, 1976