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How rapidly can ice sheets retreat? ...
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How rapidly can ice sheets retreat?
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Quaternary evolution of the northern North Sea margin through glacigenic debris-...
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Quaternary evolution of the northern North Sea margin through glacigenic debris‐...
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Glacial landforms reveal dynamic ice-sheet behaviour along the mid-Norwegian mar...
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The morphology of pockmarks on the north-east Antarctic Peninsula continental sh...
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Rapid, buoyancy-driven ice-sheet retreat of hundreds of metres per day.
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Rapid, buoyancy-driven ice-sheet retreat of hundreds of metres per day. ...
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The configuration of Northern Hemisphere ice sheets through the Quaternary
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The configuration of Northern Hemisphere ice sheets through the Quaternary
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The configuration of Northern Hemisphere ice sheets through the Quaternary
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The configuration of Northern Hemisphere ice sheets through the Quaternary
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The configuration of Northern Hemisphere ice sheets through the Quaternary. ...
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The configuration of Northern Hemisphere ice sheets through the Quaternary.
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Sea-floor and sea-ice conditions in the western Weddell Sea, Antarctica, around...
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Anvers-Hugo Trough palaeo-ice stream, Antarctic Peninsula: geomorphological evid...
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Subglacial Hydrological Control on Flow of an Antarctic Peninsula Palaeo-ice Str...
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Subglacial Hydrological Control on Flow of an Antarctic Peninsula Palaeo-ice Str...
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Subglacial hydrological control on flow of an Antarctic Peninsula palaeo-ice str...
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Subglacial hydrological control on flow of an Antarctic Peninsula palaeo-ice str...
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