Tracing the Sveconorwegian orogen into the Caledonides of West Norway: Geochronological and isotopic studies on magmatism and migmatization-Reference-Cited by-同舟云学术

Tracing the Sveconorwegian orogen into the Caledonides of West Norway: Geochronological and isotopic studies on magmatism and migmatization

Published:2021-08 Issue: Volume:362 Page:106301
ISSN:0301-9268
Container-title:Precambrian Research
language:en
Short-container-title:Precambrian Research

Author:

Wang Cheng-Cheng,Wiest Johannes D.,Jacobs Joachim,Bingen Bernard,Whitehouse Martin J.,Elburg Marlina A.,Sørstrand Thea S.,Mikkelsen Lise,Hestnes Åse

Funder

University of Bergen

Research Council of Norway

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference157 articles.

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2. Deep crustal fabrics and a model for the extensional collapse of the southwest Norwegian Caledonides;Andersen;J. Struct. Geol.,1994

3. Nature and distribution of deep crustal reservoirs in the southwestern part of the Baltic Shield: evidence from Nd, Sr and Pb isotope data on late Sveconorwegian granites;Andersen;J. Geol. Soc.,2001

4. Crustal evolution in the SW part of the Baltic Shield: the Hf isotope evidence;Andersen;J. Petrol.,2002

5. Sveconorwegian crustal underplating in southwestern Fennoscandia: LAM-ICPMS U-Pb and Lu–Hf isotope evidence from granites and gneisses in Telemark, southern Norway;Andersen;Lithos,2007

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