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: | , , |
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Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Geological Society of London
2016
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Subjects: | |
Online Access: | https://www.repository.cam.ac.uk/handle/1810/253397 |