Crustal-scale rheological transitions during late-orogenic collapse
- 1 June 2001
- journal article
- Published by Elsevier in Tectonophysics
- Vol. 335 (1-2), 211-228
- https://doi.org/10.1016/s0040-1951(01)00053-1
Abstract
No abstract availableKeywords
This publication has 66 references indexed in Scilit:
- Strain patterns within the late Variscan granitic dome of Velay, French Massif CentralJournal of Structural Geology, 1994
- Structures and way-up criteria in migmatites, with application to the Velay dome (French Massif Central)Journal of Structural Geology, 1993
- Asymmetrical pull-aparts and foliation fish as kinematic indicatorsJournal of Structural Geology, 1986
- Obduction, backfolding and piggyback thrusting in the metamorphic hinterland of the southeastern Canadian CordilleraJournal of Structural Geology, 1986
- The southeastern Canadian Cordillera: Thrust faulting, tectonic wedging, and delamination of the lithosphereJournal of Structural Geology, 1986
- Porphyroclast systems as kinematic indicatorsJournal of Structural Geology, 1986
- Structural evolution of the Thor-Odin gneiss domeTectonophysics, 1984
- Columbia River fault zone: southeastern margin of the Shuswap and Monashee complexes, southern British ColumbiaCanadian Journal of Earth Sciences, 1981
- Orthogneiss, mylonite and non coaxial deformation of granites: the example of the South Armorican Shear ZoneJournal of Structural Geology, 1979
- Critical phenomena in the rheology of partially melted rocksTectonophysics, 1978