Quelques Caractéristiques Géologiques et Minéralogiques des Dépôts d'Argile du Nord-Ouest du Québec
The clay deposits of Northwestern Quebec (from Matagami to Rupert House) were formed during the retreat of the Laurentian ice sheet. The oldest deposits are varved clays formed when the region was submerged by glacial Lake Barlow – Ojibway; the varved clays have been traced northward to Rupert House...
Published in: | Canadian Journal of Earth Sciences |
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Main Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Canadian Science Publishing
1971
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Subjects: | |
Online Access: | http://dx.doi.org/10.1139/e71-142 http://www.nrcresearchpress.com/doi/pdf/10.1139/e71-142 |