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...
Published in: | Journal of Metamorphic Geology |
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Main Authors: | , , |
Format: | Text |
Language: | unknown |
Published: |
DigitalCommons@CalPoly
2015
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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 |