Petrology of the Fort Smith - Great Slave Lake radiometric high near Pilot Lake, N.W.T.

Near Pilot Lake, the east boundary of the Fort Smith – Great Slave Lake radiometric high coincides with the contact of a well-foliated, porphyroblastic microcline–plagioclase–quartz-garnet–biotite gneiss 1 (Pilot Lake Gneiss) with a hybrid assemblage of quartzite, mica schist, garnet–cordierite gnei...

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Bibliographic Details
Published in:Canadian Journal of Earth Sciences
Main Authors: Burwash, R. A., Cape, D. F.
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1981
Subjects:
Online Access:http://dx.doi.org/10.1139/e81-081
http://www.nrcresearchpress.com/doi/pdf/10.1139/e81-081