Deep crustal fabrics and a model for the extensional collapse of the southwest Norwegian Caledonides
- 14 April 2003
- journal article
- Published by Elsevier
- Vol. 16 (9) , 1191-1203
- https://doi.org/10.1016/0191-8141(94)90063-9
Abstract
No abstract availableKeywords
This publication has 40 references indexed in Scilit:
- Petrological constraints and PT path of Devonian collapse tectonics within the Scandian mountain belt (Western Gneiss Region, Norway)Journal of the Geological Society, 1992
- Structural development and petrofabrics of eclogite facies shear zones, Bergen Arcs, western Norway: implications for deep crustal deformational processesJournal of Metamorphic Geology, 1992
- Mineral-fluid-melt interactions in high-pressure shear zones in the Bergen Arcs nappe complex, Caledonides of W. Norway: Implications for the fluid regime in Caledonian eclogite-facies metamorphismLithos, 1991
- Subduction and eduction of continental crust: major mechanisms during continent‐continent collision and orogenic extensional collapse, a model based on the south Norwegian CaledonidesTerra Nova, 1991
- The granulite-eclogite facies transition: A comparison of experimental work and a natural occurrence in the Bergen Arcs, western NorwayLithos, 1990
- Uplift of deep crust during orogenic extensional collapse: A model based on field studies in the Sogn‐Sunnfjord Region of western NorwayTectonics, 1990
- The Sunnfjord Melange, evidence of Silurian ophiolite accretion in the West Norwegian CaledonidesJournal of the Geological Society, 1990
- Extensional collapse of orogensTectonics, 1988
- Eclogitization of lower crustal granulites by fluid migration through shear zonesEarth and Planetary Science Letters, 1987
- Shear-zone model for the origin of metamorphic core complexesGeology, 1983