Sediment movement and dispersal patterns on the Grand Banks continental shelf and slope were tied to the dynamics of the Laurentide ice-sheet margin

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ADS bibcode: 2015AGUFMEP11A..03R
year: 2015
Listed Authors: Rashid, H.; MacKillop, K.; Piper, D.; Vermooten, M.; Higgins, J.; Marche, B.; Langer, K.; Brockway, B.; Spicer, H. E.; Webb, M. D.; Fournier, E.
Listed Institutions: Memorial University of Newfoundland Grenfell, Corner Brook, NL, Canada; Bedford Institute of Oceanography, Dartmouth, NS, Canada; Bedford Institute of Oceanography, Dartmouth, NS, Canada; Memorial University of Newfoundland Grenfell, Corner Brook, Canada; Bedford Institute of Oceanography, Dartmouth, NS, Canada; Memorial University of Newfoundland Grenfell, Corner Brook, Canada; Memorial University of Newfoundland Grenfell, Corner Brook, Canada; Memorial University of Newfoundland Grenfell, Corner Brook, Canada; Memorial University of Newfoundland Grenfell, Corner Brook, Canada; Memorial University of Newfoundland Grenfell, Corner Brook, Canada; Memorial University of Newfoundland Grenfell, Corner Brook, Canada

Sediment movement and dispersal patterns on the Grand Banks continental shelf and slope were tied to the dynamics of the Laurentide ice-sheet margin

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