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...
Main Authors: | , , , , , , , , |
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Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
1998
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Subjects: | |
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 http://www.scopus.com/inward/record.url?scp=0032322825&partnerID=8YFLogxK |