Xenoliths reveal a hot Moho and thin lithosphere at the Cordillera-craton boundary of western Canada
Author:
Affiliation:
1. 1School of Earth and Ocean Sciences, University of Victoria, Victoria, BC V8P 3E6, Canada
2. 2Department of Earth, Ocean and Atmospheric Sciences, University of British Columbia, Vancouver, BC V6T 1Z4, Canada
Abstract
Publisher
Geological Society of America
Subject
Geology
Link
https://pubs.geoscienceworld.org/gsa/geology/article-pdf/50/10/1135/5695174/g50151.1.pdf
Reference34 articles.
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2. Seismic evidence for lithospheric thinning and heat in the northern Canadian Cordillera;Audet;Geophysical Research Letters,2019
3. Plateau uplift in western Canada caused by lithospheric delamination along a craton edge;Bao;Nature Geoscience,2014
4. The petrology of ultramafic xenoliths from Summit Lake, near Prince George, British Columbia;Brearley;Contributions to Mineralogy and Petrology,1984
5. Petrology of ultramafic xenoliths from Rayfield River, south-central British Columbia;Canil;Canadian Journal of Earth Sciences,1987
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