Late Cretaceous bimodal magmatism,northern Ellesmere Island:isotopic age and origin

In the Yelverton Bay region of northwestern Ellesmere Island, bimodal intrusive and volcanic rocks are associated with a major fault in the Proterozoic–Cambrian rocks of the Pearya Terrane. The Wootton intrusion consists mainly of gabbro with lesser amounts of granitic and hybrid rocks; the Hansen P...

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Bibliographic Details
Published in:Canadian Journal of Earth Sciences
Main Authors: Trettin, H. P., Parrish, R.
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1987
Subjects:
Online Access:http://dx.doi.org/10.1139/e87-027
http://www.nrcresearchpress.com/doi/pdf/10.1139/e87-027