The Grenville Province

Canadian Institute of Mining, Metallurgy and Petroleum
A. J. Baer
Organization:
Canadian Institute of Mining, Metallurgy and Petroleum
Pages:
4
File Size:
2614 KB
Publication Date:
Jan 1, 1970

Abstract

"DEFINITION OF THE REGION AND ITS BOUNDARIESTHE EXPOSED PART OF THE GRENVILLE PROVINCE is the southeastern part of the Canadian Shield, characterized by crystalline rocks with K-Ar ages of about 1,000 million years. Its Canadian portion is bounded on the southwest by Georgian Bay •and by Paleozoic sediments south of a line passing through Orillia and Kingston, on the southeast by the St. Lawrence River valley and the north shore of the Gulf of the St. Lawrence, on the east by the coast of Labrador and on the northwest by the Grenville front, a linear tec-tonic feature that is a metamorphic transition zone and/or a fault. Rocks located to the southeast of the front have younger K-Ar radiom€tric ages than rocks located to the northwest of it.The region is formed of complexly deformed and highly metamorphosed crystalline rocks and in part differs from other areas of the Canadian Shield by the presence of large amounts of crystalline limestone and bodies of anorthosite."
Citation

APA: A. J. Baer  (1970)  The Grenville Province

MLA: A. J. Baer The Grenville Province. Canadian Institute of Mining, Metallurgy and Petroleum, 1970.

Export
Purchase this Article for $25.00

Create a Guest account to purchase this file
- or -
Log in to your existing Guest account