Bottom current control on sediment deposition between the Iselin bank and the Hillary canyon (Antarctica) since the late Miocene: An integrated seismic- oceanographic approach

Authors

M. Rebesco, National Institute of Oceanography and Applied Geophysics
R. Conte, Ca' Foscari University of Venice
Santis L De
F. Colleoni, National Institute of Oceanography and Applied Geophysics
M. Bensi, National Institute of Oceanography and Applied Geophysics
A. Bergamasco, National Research Council of Italy
V. Kovacevic, National Institute of Oceanography and Applied Geophysics
J. Gales, School of Biological and Marine Sciences
F. Zgur, National Institute of Oceanography and Applied Geophysics
D. Accettella, National Institute of Oceanography and Applied Geophysics
Steur L De
L. Ursella, National Institute of Oceanography and Applied Geophysics
R. McKay, Victoria University of Wellington
S. Kim, Korea Polar Research Institute
R. G. Lucchi, National Institute of Oceanography and Applied Geophysics

ORCID

• J. Gales: 0000-0003-4402-5800

DOI Link

10.1016/j.dsr.2021.103606

DOI

10.1016/j.dsr.2021.103606

Publication Date

2021-08-05

Publication Title

Deep Sea Research Part I: Oceanographic Research Papers

ISSN

0967-0637

Embargo Period

2022-08-05

Recommended Citation

Rebesco, M., Conte, R., De, S., Colleoni, F., Bensi, M., Bergamasco, A., Kovacevic, V., Gales, J., Zgur, F., Accettella, D., De, S., Ursella, L., McKay, R., Kim, S., & Lucchi, R. (2021) 'Bottom current control on sediment deposition between the Iselin bank and the Hillary canyon (Antarctica) since the late Miocene: An integrated seismic- oceanographic approach', Deep Sea Research Part I: Oceanographic Research Papers, . Available at: 10.1016/j.dsr.2021.103606