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...
Published in: | Canadian Journal of Earth Sciences |
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Format: | Article in Journal/Newspaper |
Language: | English |
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Canadian Science Publishing
1983
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Online Access: | http://dx.doi.org/10.1139/e83-161 http://www.nrcresearchpress.com/doi/pdf/10.1139/e83-161 |