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...

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Bibliographic Details
Published in:Canadian Journal of Earth Sciences
Main Author: Fyson, W. K.
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1987
Subjects:
Online Access:http://dx.doi.org/10.1139/e87-068
http://www.nrcresearchpress.com/doi/pdf/10.1139/e87-068