Regional depth-controlled hydrothermal metamorphism in the Zymoetz River area, British Columbia

An estimated 6 km of basic to silicic volcanic flows and clastic rocks of the Early Jurassic Telkwa Formation is exposed in moderately east-dipping fault blocks along the Zymoetz River, British Columbia. Extensive wholesale zeolitic replacement of porous tuff beds suggests widespread hydrothermal ac...

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Bibliographic Details
Published in:Canadian Journal of Earth Sciences
Main Authors: Mihalynuk, M. G., Ghent, E. D.
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1996
Subjects:
Online Access:http://dx.doi.org/10.1139/e96-088
http://www.nrcresearchpress.com/doi/pdf/10.1139/e96-088