A succession of quartz veins in Archean metaturbidites, Yellowknife Bay, Slave Province
The style of extensional quartz veins changed during deformation and metamorphism of greywacke–mudstones near Yellowknife, with successive types of veins accompanying a progression from steeply plunging, predominantly macroscopic F 1 , and F 2 folds to mesoscopic F 3 folds and subvertical S 3 axial...
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
1987
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Online Access: | http://dx.doi.org/10.1139/e87-068 http://www.nrcresearchpress.com/doi/pdf/10.1139/e87-068 |