Post-Ophiolite Unconformity, Tilt Cove – Betts Cove Area, Newfoundland
Subaerial sediments and silicic and mafic lavas of the Cape St. John Group in northern Newfoundland, were originally interpreted as younger than the Betts Cove ophiolite suite and the Lower Ordovician (Arenig) Snooks Arm pillow lavas and oceanic sediments, but recently have been considered as part o...
Published in: | Canadian Journal of Earth Sciences |
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Main Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Canadian Science Publishing
1975
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Subjects: | |
Online Access: | http://dx.doi.org/10.1139/e75-077 http://www.nrcresearchpress.com/doi/pdf/10.1139/e75-077 |