Structural evolution of a section along the base of the St. Anthony Complex, northwest Newfoundland

The basal portion of the St. Anthony Complex is made up of structural slices 10–30 m thick, with unknown amounts of relative movement between them. The lowest rocks are variably deformed pillow lavas and related rocks with one pervasive foliation. These rocks are overlain by greenschists, phyllonite...

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Bibliographic Details
Published in:Canadian Journal of Earth Sciences
Main Author: Craw, D.
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1983
Subjects:
Online Access:http://dx.doi.org/10.1139/e83-161
http://www.nrcresearchpress.com/doi/pdf/10.1139/e83-161