Glacial-driven Turbidity Currents
Glacial-Driven Turbidity Currents is a type of sediment gravity flow initiated by the sudden release of glacially derived sediments into marine environments, distinguished by its direct linkage to glacial processes such as iceberg calving, meltwater discharge, or subglacial sediment-laden outburst floods.
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RATIONAL THEORY OF DELTA FORMATION
Charles C. Bates · AAPG Bulletin · 1953 · 479 citations
Grand Banks Slump: GEOLOGICAL NOTES
Bruce C. Heezen, Charles L. Drake · AAPG Bulletin · 1964 · 70 citations
Julian A. Dowdeswell, Colm Ó Cofaigh, J. Taylor et al. · Geological Society London Special Publications · 2002 · 67 citations
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Geological Survey of Canada
Ottawa, Canada
4 h-index
6 publications
148 citations
Ifremer
Brest, France
3 h-index
12 publications
529 citations
Queen's University
Kingston, Canada
3 h-index
6 publications
143 citations
Natural Resources Canada
Ottawa, Canada
3 h-index
4 publications
83 citations

Centre National de la Recherche Scientifique
Paris, France
2 h-index
2 publications
57 citations

National Oceanography Centre
Southampton, United Kingdom
2 h-index
4 publications
118 citations

Durham University
Durham, United Kingdom
2 h-index
7 publications
151 citations
Washington Center
Washington, United States
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1 publications
479 citations
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JG · 3 publications · 125 citations
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2 publications · 549 citations
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2 publications · 71 citations
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1 publications · 40 citations
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1 publications · 67 citations
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