the Geology of an Area Between Pigou and Sheldrake Rivers, Saguenay County, Quebec, with a Detailed Study of the Anorthosites.
The area is on the north shore of the Gulf of St. Lawrence, 325 miles below Quebec. The consolidated rocks are all of Pre-cambrian age. In order of abundance they are:- anorthositic and gabbroic rocks, granitic intrusives, syenitic rocks, paragneisses, amphibolites, migmatites, dioritic intrusives,...
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| Format: | Others |
| Language: | en |
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McGill University
1956
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| Online Access: | http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=110227 |
| Summary: | The area is on the north shore of the Gulf of St. Lawrence, 325 miles below Quebec. The consolidated rocks are all of Pre-cambrian age. In order of abundance they are:- anorthositic and gabbroic rocks, granitic intrusives, syenitic rocks, paragneisses, amphibolites, migmatites, dioritic intrusives, and various minor intrusives. The paragneisses have been called Grenville by earlier workers. [...] |
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