Complex evolution of folds and cleavages in Archean rocks, Yellowknife, N.W.T.

Overturned folds and later cleavages in a metasedimentary terrain with marginal volcanics near Yellowknife form a complex succession in which structures repeatedly trend eastward and northward. Early major east–west folds are overturned away from a southern granodioritic complex and terminate westwa...

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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 1982
Subjects:
Online Access:http://dx.doi.org/10.1139/e82-073
http://www.nrcresearchpress.com/doi/pdf/10.1139/e82-073