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Runway Site Survey,
Pensacola
Mountains, Antarctica.
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Subglacial geology and geomorphology of the
Pensacola
‐Pole Basin, East Antarctica
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Subglacial Geology and Geomorphology of the
Pensacola
‐Pole Basin, East Antarctica
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Subglacial geology and geomorphology of the
Pensacola
-Pole Basin, East Antarctica.
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Subglacial Geology and Geomorphology of the
Pensacola
-Pole Basin, East Antarctica
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Palaeozoic to Mesozoic polyphase deformation of the Patuxent Range,
Pensacola
Mountains, Antarctica
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Palaeozoic to Mesozoic polyphase deformation of the Patuxent Range,
Pensacola
Mountains, Antarctica
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Processed line aerogravity data over the Dufek Massif,
Pensacola
Mountains (1997/99 season)
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Processed line aeromagnetic data over the Dufek Massif,
Pensacola
Mountains (1998/99 season)
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Culturable diversity of heterotrophic bacteria in Forlidas Pond (
Pensacola
Mountains) and Lundstrom Lake (Shackleton Range), Antarctica
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Deglacial history of the
Pensacola
Mountains, Antarctica from glacial geomorphology and cosmogenic nuclide surface exposure dating
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Deglacial history of the
Pensacola
Mountains, Antarctica from glacial geomorphology and cosmogenic nuclide surface exposure dating.
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Culturable diversity of heterotrophic bacteria in Forlidas Pond (
Pensacola
Mountains) and Lundström Lake (Shackleton Range), Antarctica
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Processed bed elevation picks from the POLARGAP radar survey across the
Pensacola
-Pole Basin (2015/2016)
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Processed bed elevation picks from airborne radar depth sounding across the Dufek Massif,
Pensacola
Mountains (1998/99 season)
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Latest Neoproterozoic to Mid-Cambrian age for the main deformation phases of the Transantarctic Mountains: new stratigraphic and isotopic constraints from the
Pensacola
Mountains, Antarctica
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Lake highstands in the
Pensacola
Mountains and Shackleton Range 4300-2250 cal. yr BP: Evidence of a warm climate anomaly in the interior of Antarctica
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Latest neoproterozoic to Mid-Cambrian age for the main deformation phases of the transantarctic mountains: New stratigraphic and isotopic constraints from the
Pensacola
mountains, Antarctica
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Latest Neoproterozoic to Mid-Cambrian age for the main deformation phases of the Transantarctic Mountains: new stratigraphic and isotopic constraints from the
Pensacola
Mountains, Antarctica
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Lake highstands in the
Pensacola
Mountains and Shackleton Range 4300–2250 cal. yr BP: Evidence of a warm climate anomaly in the interior of Antarctica
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Occdownload Gbif.Org
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Peeters, Karolien
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Willems, Anne
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Baldwin, Amy J.
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Catala, Philippe
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Hein, Andrew S.
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Jeffrey, Wade H.
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Joux, Fabien
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Matsuoka, Kenichi
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Moss, Joseph A.
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Pakulski, Joseph D.
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Balco, Greg
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Eagles, Graeme
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Ertz, Damien
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Ferraccioli, Fausto
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Fetter, A. H.
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Forsberg, René
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Goehring, Brent M.
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Jordan, Tom A.
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Nichols, Keir A.
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Ross, Neil
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Rowell, A. J.
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Storey, B. C.
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Todd, Claire
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Verleyen, Elie
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A. S. Hein
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biodiversity
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Antarctica
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BAROMETRIC PRESSURE
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[SDU.OCEAN]Sciences of the Universe [physics]/Ocean
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cultivation
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A. OTKUPTSCHIKOV
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343
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Australian Antarctic Division
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