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1. Glacigenic sediment dynamics and climatically controlled submarine landslides on the NW Barents Sea margin

Author

Rebesco, Michele, Lucchi, Renata G., Camerlenghi, Angelo, Urgeles, Roger, Accettella, Daniela, De Mol, Ben, Sauli, Chiara, Pedrosa, M.T., Madrussani, Gianni, and Llopart, Jaume

Abstract

The Deep-sea & Sub-Seafloor Frontiers Conference project (DS3F), 11-14 March 2012, Sitges, Barcelona, Spain, At high-latitudes, sediment dynamics and consequent continental margin architecture are deeply affected by grounded ice. Fast-flowing ice streams deliver large quantities of sediments from meltwater plumes and Glacigenic Debris Flows (GDFs) at the mouth of cross-shelf troughs during relatively short time periods (deglaciations and glacial maxima, respectively). Glacigenic sediment dynamics also controls the distribution in time and space of large-scale landslides

Published
2012

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