Glaciomarine sediment deposition on the continental slope and rise of the central Ross Sea since the Last Glacial Maximum

The continental margin of the Ross Sea has been consistently sensitive to the advance and retreat of the Ross Ice Sheet (RIS) between the interglacial and glacial periods. This study examines changes of the glaciomarine sedimentation on the continental slope and rise to the eastern side of Hillary C...

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Bibliographic Details
Published in:Marine Geology
Main Authors: Ha S., Colizza E., Torricella F., Langone L., Giglio F., Kuhn G., Macri P., Khim B. -K.
Other Authors: Ha, S., Colizza, E., Torricella, F., Langone, L., Giglio, F., Kuhn, G., Macri, P., Khim, B. -K.
Format: Article in Journal/Newspaper
Language:English
Published: 2022
Subjects:
Online Access:http://hdl.handle.net/11368/3017404
https://doi.org/10.1016/j.margeo.2022.106752