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Cordilleria, a newly defined Canadian microcontinent

Nature volume 314, pages 707–713 (1985)Cite this article

Abstract

Palaeomagnetic data and geological field evidence indicate that most of the western Canadian cordillera lay 1,500 km south of its present position in the early Cretaceous. We suggest that this region comprised a microcontinent, termed Cordilleria, which moved on the Kula plate and collided with the craton ˜100 Myr ago to form first the Mackenzie Mountains and then the Rockies.

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Authors and Affiliations

  1. Department of Geology, The University of Alberta, Edmonton, Alberta, Canada, T6G 2E3

    V. E. Chamberlain & R. St J. Lambert

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  1. V. E. Chamberlain
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  2. R. St J. Lambert
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Chamberlain, V., Lambert, R. Cordilleria, a newly defined Canadian microcontinent. Nature 314, 707–713 (1985). https://doi.org/10.1038/314707a0

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