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A large West Antarctic Ice Sheet explains early Neogene sea-level amplitude
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A large West Antarctic Ice Sheet explains early Neogene sea-level amplitude
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A large West Antarctic Ice Sheet explains early Neogene sea-level amplitude
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A large West Antarctic Ice Sheet explains early Neogene sea-level amplitude
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A large West Antarctic Ice Sheet explains early Neogene sea-level amplitude
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A large West Antarctic Ice Sheet explains early Neogene sea-level amplitude
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A large West Antarctic Ice Sheet explains early Neogene sea-level amplitude
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The Southern Ocean observing system: Initial science and implementation strategy
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Chapter 10 - Pleistocene Antarctic climate variability: ice sheet – ocean – clim...
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Late Pleistocene and Holocene Sedimentation of the George V Continental Shelf, E...
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Continental Shelf Record of the East Antarctic Ice Sheet Evolution: Seismo-strat...
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A New High-resolution Depth Model for the Terre Adélie and George V Shelf and M...
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Sedimenary Processes in the Wilkes Land Margin: A Record of Cenozoic East Antarc...
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Ice shelf grounding zone features of western Prydz Bay, Antarctica sedimentary p...
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Physical Controls on Coral Communities on the George V Land Slope: Some Working...
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Physical Controls on Deep Water Coral Communities on the George V Land Slope, Ea...
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Antarctic CRC Marine Geoscience, Vincennes Bay, Prydz Bay and Mac.Robertson Shel...
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The Odyssea Drift (Ross Sea, Antarctica).
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