The Gwillim Gold Mine and Its Geological Setting

Canadian Institute of Mining, Metallurgy and Petroleum
G. Bouchard J. Guha W. Zuckerk el J. Carignan G. Archambault
Organization:
Canadian Institute of Mining, Metallurgy and Petroleum
Pages:
8
File Size:
2791 KB
Publication Date:
Jan 1, 1984

Abstract

The Gwillim Mine, located 8 km northwest of Chibougamau, is underlain by two mafic volcanic cycles separated by a dominantly felsic cycle. These rocks are part of the Gilman Formation of the Roy Group. The mafic rocks are cut by weak shear zones containing the "North" and "Main" veins, both east-west striking gold-bearing structures dipping 75° to the north. The felsic cycle, which is also gold-bearing, contains textures suggesting a syngenetic origin. The Gwillim Mine presents an excellent opportunity for the study of what may be two coexisting gold deposits, a volcanogenic and a veine type.
Citation

APA: G. Bouchard J. Guha W. Zuckerk el J. Carignan G. Archambault  (1984)  The Gwillim Gold Mine and Its Geological Setting

MLA: G. Bouchard J. Guha W. Zuckerk el J. Carignan G. Archambault The Gwillim Gold Mine and Its Geological Setting . Canadian Institute of Mining, Metallurgy and Petroleum, 1984.

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