Structure of the (ultra)high-pressure Western Gneiss Region, Norway: Imbrication during Caledonian continental margin subduction
Author:
Affiliation:
1. School of Earth Sciences, The Ohio State University, Columbus, Ohio 43210, USA
Publisher
Geological Society of America
Subject
Geology
Link
https://pubs.geoscienceworld.org/gsa/gsabulletin/article-pdf/130/5-6/926/4137558/926.pdf
Reference123 articles.
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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. Evidence for hyperextension along the pre-Caledonian margin of Baltica;Andersen;Journal of the Geological Society [London],2012
4. Geologisk Kart over Norge, Berggrunnskart Kristiansund M;Askvik;Trondheim, Norges Geologiske Undersøkelse, scale,1985
5. Strain within the ultrahigh-pressure Western Gneiss Region of Norway recorded by quartz CPOs;Barth,2010
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