Canyons and slides on the continental slope seaward of a shallow bank, Labrador margin, eastern Canada
The ~ 200 km-wide Labrador continental shelf consists of a series of shallow banks and intervening cross-shelf troughs (Fig. 1b). Glacial reconstructions suggest that the banks were occupied by slow-flowing ice and the troughs by ice-streams during several Quaternary glaciations (Dyke et al. 2002; J...
| Main Authors: | , , |
|---|---|
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
Geological Society of London
2016
|
| Subjects: | |
| Online Access: | https://www.repository.cam.ac.uk/handle/1810/253397 |