Migmatite gneiss of the Jættedal complex, Liverpool Land, East Greenland: protracted high‐ T metamorphism in the overriding plate of the Caledonian orogen

Abstract The Greenland Caledonides (GC) formed in the overriding Laurentian plate during the closure of the Iapetus Ocean and the subduction of Baltica, and offer a unique opportunity to study metamorphic patterns, regional structures and the kinematic evolution of the overriding plate of a continen...

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Bibliographic Details
Published in:Journal of Metamorphic Geology
Main Authors: Johnston, S. M., Kylander‐Clark, A., Brueckner, H. K.
Other Authors: NSF-EAR
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2015
Subjects:
Online Access:http://dx.doi.org/10.1111/jmg.12167
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fjmg.12167
https://onlinelibrary.wiley.com/doi/pdf/10.1111/jmg.12167