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...

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Bibliographic Details
Published in:Canadian Journal of Earth Sciences
Main Authors: Ballivy, Gérard, Pouliot, Gaston, Loiselle, André
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1971
Subjects:
Online Access:http://dx.doi.org/10.1139/e71-142
http://www.nrcresearchpress.com/doi/pdf/10.1139/e71-142