Prolonged post-orogenic extension in the southeastern Canadian Cordillera: Miocene reactivation of the Columbia River Fault

Author:

Damant Kade A.,Enkelmann Eva,Jess Scott

Funder

University of Calgary

Natural Sciences and Engineering Research Council of Canada

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference94 articles.

1. Cordilleran metamorphic core complexes - from Arizona to Southern Canada;Armstrong;Annu. Rev. Earth Planet. Sci.,1982

2. Cenozoic Cooling Patterns from the Canadian Cordillera using the Uranium-Thorium-Helium Method;Bacque,2013

3. Plateau uplift in western Canada caused by lithospheric delamination along a craton edge;Bao;Nat. Geosci.,2014

4. Kinematic interpretation of mylonitic rocks in part of the Columbia River fault zone, Shuswap terrane, British Columbia;Brown;Canadian Journal of Earth Sciences,1982

5. Tectonic denudation of the Shuswap metamorphic terrane of southeastern British Columbia;Brown;Geology,1987

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