A glacier-influenced turbidite system and associated landform assemblage in the Greenland Basin and adjacent continental slope

• Published in: Geological Society, London, Memoirs
• Main Authors: Garcia, M., Batchelor, C. L., Dowdeswell, J. A., Hogan, K. A., O Cofaigh, C.
• Other Authors: Dowdeswell, J.A., Canals, M., Jakobsson, M., Todd, B.J., Dowdeswell, E.K., Hogan, K.A.
• Format: Book Part
• Language: unknown
• Published: Geological Society of London 2016
• Subjects: Greenland; Greenland Basin; glacier; Ice Sheet
• Online Access: http://nora.nerc.ac.uk/id/eprint/515714/; https://doi.org/10.1144/M46.148

Evidence of the former extent and dynamics of the Greenland Ice Sheet is preserved on the continental margin of NE Greenland (Fig. 1). The continental shelf is incised by a number of deep (up to 500 m) cross-shelf troughs (Batchelor & Dowdeswell 2014; Arndt et al. 2015) (Fig. 1a), which are inte...