• Geomorphology and development of a high-latitude channel system: the INBIS channel case (NW Barents Sea, Arctic) 

      Rui, L.; Rebesco, M.; Casamor, J.L.; Laberg, Jan Sverre; Rydningen, Tom Arne; Caburlotto, A.; Forwick, Matthias; Urgeles, R.; Accettella, D.; Lucchi, R. G.; Delbono, I.; Barsanti, M.; Demarte, M.; Ivaldi, R. (Journal article; Tidsskriftartikkel; Peer reviewed, 2019-02-25)
      The INBIS (Interfan Bear Island and Storfjorden) channel system is a rare example of a deep-sea channel on a glaciated margin. The system is located between two trough mouth fans (TMFs) on the continental slope of the NW Barents Sea: the Bear Island and the Storfjorden–Kveithola TMFs. New bathymetric data in the upper part of this channel system show a series of gullies that incise the shelf break ...
    • Recognizing key sedimentary facies and their distribution in mixed turbidite–contourite depositional systems: The case of the Pacific margin of the Antarctic Peninsula 

      Rodrigues, Sara; Hernández-Molina, F. J.; Hillenbrand, C.-D.; Lucchi, Renata Giulia; Rodríguez-Tovar, F. J.; Rebesco, M.; Larter, R.D. (Journal article; Tidsskriftartikkel; Peer reviewed, 2022-02-01)
      Interplay of deep-water sedimentary processes is responsible for building a myriad of features and deposits across mixed turbidite–contourite systems, from <5 cm beds to >200 km long sedimentary drifts. Investigations of the spatial and temporal variability of their sedimentary facies and facies associations is crucial to reveal the dynamics between along-slope bottom currents and down-slope turbidity ...