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

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 continental colli...

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Bibliographic Details
Published in:Journal of Metamorphic Geology
Main Authors: Johnston, S. M., Kylander-Clark, A., Brueckner, H. K.
Format: Text
Language:unknown
Published: DigitalCommons@CalPoly 2015
Subjects:
Online Access:https://digitalcommons.calpoly.edu/phy_fac/481
https://doi.org/10.1111/jmg.12167
https://digitalcommons.calpoly.edu/context/phy_fac/article/1490/viewcontent/JohnstonS_2015_MigmatiteGneissJaettedal.pdf