Post-LGM glaciomarine processes revealed by inner shelf sedimentary facies analysis (Terra Nova Bay, Western Ross Sea, Antarctica)-Reference-Cited by-同舟云学术

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Post-LGM glaciomarine processes revealed by inner shelf sedimentary facies analysis (Terra Nova Bay, Western Ross Sea, Antarctica)

Published:2024-07 Issue: Volume:697 Page:64-77
ISSN:1040-6182
Container-title:Quaternary International
language:en
Short-container-title:Quaternary International

Author:

Giorgetti Giulia^ORCID,Baroni Carlo^ORCID,Salvatore Maria Cristina^ORCID,Gasperini Luca,Polonia Alina

Publisher

Elsevier BV

Reference74 articles.

1. Subdecadally resolved paleoceanography of the Peru margin during the last two millennia;Agnihotri;G-cubed,2008

2. Till beneath Ice Stream B. 3. Till deformation: evidence and implications;Alley;J. Geophys. Res.,1987

3. Sedimentation beneath ice shelves — the view from ice stream B;Alley;Mar. Geol.,1989

4. Sedimentation on the Ross Sea continental shelf, Antarctica;Anderson;Mar. Geol.,1984

5. Sedimentary facies associated with Antarctica's floating ice masses;Anderson,1991

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