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...

Full description

Bibliographic Details
Published in:Canadian Journal of Earth Sciences
Main Authors: Neale, E. R. W., Kean, B. F., Upadhyay, H. D.
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1975
Subjects:
Online Access:http://dx.doi.org/10.1139/e75-077
http://www.nrcresearchpress.com/doi/pdf/10.1139/e75-077