Present and postglacial rates of uplift for glaciated northern and eastern North America derived from postglacial uplift curves
Average rates of postglacial uplift reach a maximum value of nearly 4 m 100 y −1 over southeastern Hudson Bay, and another high cell, with rates of about 2.5 m 100 y −1 , lies between Bathurst Inlet and Southampton Island. Current rates of uplift are underestimated if exponential curves are fitted s...
Published in: | Canadian Journal of Earth Sciences |
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Main Author: | |
Format: | Article in Journal/Newspaper |
Language: | English |
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Canadian Science Publishing
1970
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Online Access: | http://dx.doi.org/10.1139/e70-069 http://www.nrcresearchpress.com/doi/pdf/10.1139/e70-069 |