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This study reviews the stratigraphic architecture of the Cenozoic succession in the Victoria Land Basin, Antarctica, which records significant palaeoenvironmental changes over the past 34 million years. The analysis of drillcores and seismic data reveals various lithofacies that document glacial advance-retreat cycles and depositional sequences, reflecting a complex history of Antarctic glaciation. The findings highlight the importance of this region in understanding both modern climate change and long-term

Author

Sofia Carolina Avellaneda

Language

EN