Evolution of the Appalachian laurentian margin: Lithoprobe results in western Newfoundland

The Humber Zone of the western Newfoundland Appalachians represents the early Paleozoic Laurentian margin established by Neoproterozoic rifting. After a period of passive margin thermal subsidence, Taconian deformation began in the Early Ordovician with westward thrusting. Subsequently, an extensive...

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Bibliographic Details
Main Authors: Waldron, J W F, Anderson, S D, Cawood, Peter Anthony, Goodwin, L B, Hall, J, Jamieson, R A, Palmer, S E, Stockmal, C S, Williams, P F
Format: Article in Journal/Newspaper
Language:English
Published: 1998
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Online Access:https://research-portal.st-andrews.ac.uk/en/researchoutput/evolution-of-the-appalachian-laurentian-margin-lithoprobe-results-in-western-newfoundland(668a22ff-5f6d-45bd-8fb3-fe21f30ca4d7).html
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