The Pelican Thrust Zone: basal detachment between the Archean Sask Craton and Paleoproterozoic Flin Flon – Glennie Complex, western Trans-Hudson Orogen
- 1 April 2005
- journal article
- Published by Canadian Science Publishing in Canadian Journal of Earth Sciences
- Vol. 42 (4) , 685-706
- https://doi.org/10.1139/e04-035
Abstract
No abstract availableKeywords
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