Coupling, decoupling and metasomatism:Evolution of crust-mantle relationships beneath NW Spitsbergen

The Bockfjord area of NW Spitsbergen (Norwegian Arctic) exposes a long history of crustal evolution, culminating in the Caledonian (400-500. Ma) orogeny; prior to the opening of the N. Atlantic Ocean, this area was part of the Laurentian (Greenland) side of the orogen. The N-striking Breibogen-Bockf...

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Bibliographic Details
Published in:Lithos
Main Authors: Griffin, W. L., Nikolic, N., O'Reilly, Suzanne Y., Pearson, N. J.
Format: Article in Journal/Newspaper
Language:English
Published: 2012
Subjects:
Online Access:https://researchers.mq.edu.au/en/publications/944a76b6-d70c-48a3-9b79-67559875a025
https://doi.org/10.1016/j.lithos.2012.03.003
http://www.scopus.com/inward/record.url?scp=84865191203&partnerID=8YFLogxK