Recurrent E - W oscillations of the ice flow confluence of the East and West Antarctic ice sheets in the central Ross Sea, Antarctica, from the Middle Miocene to the present day

Author:

Balestrieri Maria Laura,Olivetti Valerio,Chew David,Zurli Luca,Zattin Massimiliano,Drakou Foteini,Cornamusini Gianluca,Perotti Matteo

Publisher

Elsevier BV

Subject

Paleontology,Earth-Surface Processes,Ecology, Evolution, Behavior and Systematics,Oceanography

Reference68 articles.

1. Plio-Pleistocene seismic stratigraphy of the Ross Sea: Evidence for multiple ice sheet grounding episodes, in Elliot, D.H;Alonso;Contributions to Antarctic research III: Antarct. Res. Ser.,1992

2. Cenozoic glacial history of the Ross Sea revealed by intermediate resolution seismic reflection data combined with drill site information;Anderson;Antarct. Paleoenviron.,1992

3. Ross Sea paleo-ice sheet drainage and deglacial history during and since the LGM;Anderson;Quat. Sci. Rev.,2014

4. Reassessment of the potential sea-level rise from a collapse of the West Antarctic Ice Sheet;Bamber;science,2009

5. Detrital age spectra of the middle Miocene to Present day glaciomarine sediments of the DSDP Leg 28 drilling;Balestrieri,2023

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