A thermomechanical model of exhumation of high pressure (HP) and ultra-high pressure (UHP) metamorphic rocks in Alpine-type collision belts
- 1 December 2001
- journal article
- Published by Elsevier BV in Tectonophysics
- Vol. 342 (1-2), 113-136
- https://doi.org/10.1016/s0040-1951(01)00158-5
Abstract
No abstract availableKeywords
This publication has 58 references indexed in Scilit:
- Extensional tectonics in the Caledonides of southern Norway, an overviewTectonophysics, 1998
- Processing of crust in the root of the Caledonian continental collision zone: the role of eclogitizationTectonophysics, 1997
- Kinematic, thermal and petrological model of the Central Alps: Lepontine metamorphism in the upper crust and eclogitisation of the lower crustTectonophysics, 1997
- Fine-scale isotopic heterogeneities and fluids in the deep crust: a40Ar/39Ar laser ablation and TEM study of muscovites from a granulite-eclogite transition zoneEarth and Planetary Science Letters, 1997
- Erosion as a driving mechanism of intracontinental mountain growthJournal of Geophysical Research: Solid Earth, 1996
- Deep crustal fabrics and a model for the extensional collapse of the southwest Norwegian CaledonidesJournal of Structural Geology, 1994
- Pseudotachylytes Generated During Seismic Faulting and Eclogitization of the Deep CrustScience, 1994
- Some thermomechanical aspects of the subduction of continental 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
- Quaternary extension in southern Tibet: Field observations and tectonic implicationsJournal of Geophysical Research, 1986