U–Pb geochronology of the Bokan Mountain peralkaline granite, southeastern Alaska

The Bokan Mountain arfvedsonite–aegirine granite is the only peralkaline acid intrusion actually known on the margin of the Canadian Cordillera. It is the end product of a peralkaline magmatic evolution and is characterized by genetically associated concentrations of U and Th. The U–Pb method on zir...

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Bibliographic Details
Published in:Canadian Journal of Earth Sciences
Main Authors: Saint-Andre, Bruno de, Lancelot, Joël R., Collot, Bernard
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1983
Subjects:
Online Access:http://dx.doi.org/10.1139/e83-021
http://www.nrcresearchpress.com/doi/pdf/10.1139/e83-021