Lower to Middle Ordovician evolution of peri-Laurentian arc and backarc complexes in Iapetus: Constraints from the Annieopsquotch accretionary tract, central Newfoundland

The Annieopsquotch accretionary tract in Newfoundland is composed of a series of west-dipping structural panels, each containing remnants of ophiolitic and arc-backarc complexes of Laurentian affinity formed during the Ordovician closure of Iapetus. Panels were transferred from an upper-plate to a l...

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Bibliographic Details
Published in:Geological Society of America Bulletin
Main Authors: Zagorevski, A., Rogers, N., van Staal, C. R., McNicoll, V., Lissenberg, Cornelis Johan, Valverde-Vaquero, P.
Format: Article in Journal/Newspaper
Language:unknown
Published: Geological Society of America 2006
Subjects:
Online Access:https://orca.cardiff.ac.uk/id/eprint/9914/
https://doi.org/10.1130/B25775.1