Paleomagnetism of the komatiitic basalts of the Ottawa Islands, N.W.T.

The komatiitic basalts of the Ottawa Islands in eastern Hudson Bay are on strike with and believed to form a continuation of similar units of the Cape Smith Belt 150 km to the northeast. Units sampled in the Ottawa Islands all dip gently to the west and hence are not suitable for an internal fold te...

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Bibliographic Details
Published in:Canadian Journal of Earth Sciences
Main Authors: Buchan, K. L., Baragar, W. R. A.
Format: Article in Journal/Newspaper
Language:French
Published: Canadian Science Publishing 1985
Subjects:
General Earth and Planetary Sciences
Cape Smith
Hudson
Hudson Bay
Ottawa Islands
Online Access:http://dx.doi.org/10.1139/e85-056
http://www.nrcresearchpress.com/doi/pdf/10.1139/e85-056

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