Lower crustal high-velocity bodies along North Atlantic passive margins, and their link to Caledonian suture zone eclogites and Early Cenozoic magmatism-Reference-Cited by-同舟云学术

Lower crustal high-velocity bodies along North Atlantic passive margins, and their link to Caledonian suture zone eclogites and Early Cenozoic magmatism

Published:2016-02 Issue: Volume:670 Page:16-29
ISSN:0040-1951
Container-title:Tectonophysics
language:en
Short-container-title:Tectonophysics

Author:

Mjelde Rolf,Kvarven Trond,Faleide Jan Inge,Thybo Hans^ORCID

Funder

Research Council of Norway

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference117 articles.

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

5. EUNAseis: a seismic model for Moho and crustal structure in Europe, Greenland, and the North Atlantic region;Artemieva;Tectonophysics,2013

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