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.

Bibliographic Details
Published in:Canadian Journal of Earth Sciences
Main Authors: Riddihough, R. P., Haines, G. V., Hannaford, W.
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1973
Subjects:
General Earth and Planetary Sciences
Arctic
Arctic Basin
Online Access:http://dx.doi.org/10.1139/e73-018
http://www.nrcresearchpress.com/doi/pdf/10.1139/e73-018
Description
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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