Regional Magnetic Anomalies of the Canadian Arctic
A contoured residual map of the vertical magnetic field, observed at an altitude of 3.5 km above sea level, provides a broad view of major tectonic patterns and relations between the Canadian Shield, the Innuitian Region, and the oceanic ridges of the Arctic Basin.
| Published in: | Canadian Journal of Earth Sciences |
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| Main Authors: | , , |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
Canadian Science Publishing
1973
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| Subjects: | |
| Online Access: | https://doi.org/10.1139/e73-018 http://www.nrcresearchpress.com/doi/pdf/10.1139/e73-018 |
| Summary: | A contoured residual map of the vertical magnetic field, observed at an altitude of 3.5 km above sea level, provides a broad view of major tectonic patterns and relations between the Canadian Shield, the Innuitian Region, and the oceanic ridges of the Arctic Basin. |
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