The Chipewyan Red Granitea building stone prospect

Canadian Institute of Mining, Metallurgy and Petroleum
John D. Godfrey
Organization:
Canadian Institute of Mining, Metallurgy and Petroleum
Pages:
3
File Size:
2426 KB
Publication Date:
Jan 1, 1984

Abstract

Precambrian Shield rocks, exposed in the extreme northeast corner of Alberta, provide the only possibility for a granitic building stone development in the province. Among a wide variety of granitoid rocks in the Shield, the Chipewyan Red Granite is one of the most favourable prospects. Geological mapping and exploration has revealed two prospective sites within a major pluton situated close to navigable water. Cleaned outcrop surfaces show clearly the pattern of joints and lithologic variations within the granite at prospective quarry sites. Other features include: basic dykes, quartz veins, and sheeting fracture zanes. Systematic orthogonally arranged fracture sets and the sheeting zanes are auributed to a tectonic origin. onsystematic irregular fractures are related to surface and nearsurface processes, such as decompression through unloading .
Citation

APA: John D. Godfrey  (1984)  The Chipewyan Red Granitea building stone prospect

MLA: John D. Godfrey The Chipewyan Red Granitea building stone prospect. Canadian Institute of Mining, Metallurgy and Petroleum, 1984.

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