Assembly of the Annieopsquotch Accretionary Tract, Newfoundland Appalachians: Age and Geodynamic Constraints from Syn‐Kinematic Intrusions

The Annieopsquotch Accretionary Tract (AAT) comprises several ophiolites and arc‐back‐arc igneous complexes that were accreted to the Dashwoods microcontinent during the Ordovician Taconic orogeny. The Lloyds River Fault Zone, which separates the AAT from the Dashwoods microcontinent, yielded 40Ar/3...

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Bibliographic Details
Published in:The Journal of Geology
Main Authors: Lissenberg, Cornelis Johan, Zagorevski, Alexandre, McNicoll, Vicki J., van Staal, Cees R., Whalen, Joseph B.
Format: Article in Journal/Newspaper
Language:English
Published: University of Chicago Press 2005
Subjects:
Online Access:https://orca.cardiff.ac.uk/id/eprint/9917/
https://doi.org/10.1086/431909
https://orca.cardiff.ac.uk/id/eprint/9917/1/Lissenberg_et_al_%2805%29_-_Assembly_of_the_Annieopsquotch_Accretionary_Tract,_Newfoundland_Appalachians.pdf