Plateau uplift in western Canada caused by lithospheric delamination along a craton edge
Author:
Publisher
Springer Science and Business Media LLC
Subject
General Earth and Planetary Sciences
Link
http://www.nature.com/articles/ngeo2270.pdf
Reference29 articles.
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4. DeCelles, P. G., Ducea, M. N., Kapp, P. & Zandt, G. Cyclicity in Cordilleran orogenic systems. Nature Geosci. 2, 251–257 (2009).
5. Hyndman, R. D. & Currie, C. A. Why is the North America Cordillera high? Hot backarcs, thermal isostasy, and mountain belts. Geology 39, 783–786 (2011).
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