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...
Published in: | Canadian Journal of Earth Sciences |
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Main Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Canadian Science Publishing
1983
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Subjects: | |
Online Access: | http://dx.doi.org/10.1139/e83-021 http://www.nrcresearchpress.com/doi/pdf/10.1139/e83-021 |