The Cheticamp pluton: a Cambrian granodioritic intrusion in the western Cape Breton Highlands, Nova Scotia

The Cheticamp pluton consists of biotite granodiorite (locally megacrystic) in the north and museovite–biotite granodiorite in the south, in probable faulted contact. These two rock types, especially the biotite granodiorite, show a broad range in modal and chemical compositions. They are interprete...

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Bibliographic Details
Published in:Canadian Journal of Earth Sciences
Main Authors: Barr, Sandra M., Macdonald, Alan S., Blenkinsop, John
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1986
Subjects:
Online Access:http://dx.doi.org/10.1139/e86-156
http://www.nrcresearchpress.com/doi/pdf/10.1139/e86-156