Granitoid rocks and associated coper skarn, Whycocomagh Mountain, Cape Breton Island, Nova Scotia

Mineralized (Fe-Cu-W-Mo) skarn in the Whycocomagh Mountain area is associated with a small pluton of Devonian (402±20 Ma) age, which intruded predominantly metasedimentary rocks of the Hadrynian George River Group. The pluton consists largely of granite porphyry with a marginal granodiorite to diori...

Full description

Bibliographic Details
Published in:Atlantic Geology
Main Authors: Barr, Sandra M., Choy, R. Yip, Colwell, J. A., Oldale, H. S.
Format: Article in Journal/Newspaper
Language:English
Published: Atlantic Geoscience Society 1984
Subjects:
Online Access:https://journals.lib.unb.ca/index.php/ag/article/view/1573