Deglaciation and postglacial emergence of Northernmost Labrador.
Northern Labrador lies within the Canadian Shield, its bedrock being generally Precambrian in age or, more accurately, Archean in the area covered by this study. (Map 2) (Piloski 1954). Highly metamorphosed paragneisses and gneisses of granitic composition are the major rock-types, but granite and q...
| Main Author: | |
|---|---|
| Other Authors: | |
| Format: | Others |
| Language: | en |
| Published: |
McGill University
1962
|
| Subjects: | |
| Online Access: | http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=113704 |