North Atlantic spreading axes terminate in the continental cul-de-sacs of Baffin Bay and the Laptev Sea

In conventional plate-tectonic models, an independent Greenland plate is supposed to have drifted in the Paleogene along a transform fault through Nares Strait that links the two branches of the North Atlantic spreading system. However, this postulated structure — widely known as the Wegener Fault —...

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Bibliographic Details
Published in:Canadian Journal of Earth Sciences
Main Authors: Pulvertaft, T. Christopher R., Dawes, Peter R.
Other Authors: Murphy, Brendan
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 2011
Subjects:
Online Access:http://dx.doi.org/10.1139/e11-004
http://www.nrcresearchpress.com/doi/full-xml/10.1139/E11-004
http://www.nrcresearchpress.com/doi/pdf/10.1139/E11-004