High-temperature deformation during continental-margin subduction & exhumation: The ultrahigh-pressure Western Gneiss Region of Norway-Reference-Cited by-同舟云学术

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High-temperature deformation during continental-margin subduction & exhumation: The ultrahigh-pressure Western Gneiss Region of Norway

Published:2010-01 Issue:1-4 Volume:480 Page:149-171
ISSN:0040-1951
Container-title:Tectonophysics
language:en
Short-container-title:Tectonophysics

Author:

Hacker Bradley R.,Andersen Torgeir B.,Johnston Scott,Kylander-Clark Andrew R.C.,Peterman Emily M.,Walsh Emily O.,Young David

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference116 articles.

1. Extensional tectonics in the Caledonides of southern Norway, an overview;Andersen;Tectonophysics,1998

2. Uplift of deep crust during orogenic extensional collapse: a model based on field studies in the Sogn–Sunnfjord region of western Norway;Andersen;Tectonics,1990

3. The Sunnfjord Melange, evidence of Silurian ophiolite accretion in the West Norwegian Caledonides;Andersen;Journal of the Geological Society of London,1990

4. Subduction and eduction of continental crust: major mechanism during continent–continent collision and orogenic extensional collapse, a model based on the south Caledonides;Andersen;Terra Nova,1991

5. Deep crustal fabrics and a model for the extensional collapse of the southwest Norwegian Caledonides;Andersen;Journal of Structural Geology,1994

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