Detrital Thermochronometry Reveals That the Topography Along the Antarctic Peninsula is Not a Pleistocene Landscape

Author:

Clinger Anna E.12ORCID,Fox Matthew3,Balco Greg2,Cuffey Kurt14,Shuster David L.12

Affiliation:

1. Department of Earth and Planetary Science University of California Berkeley CA USA

2. Berkeley Geochronology Center Berkeley CA USA

3. Department of Earth Sciences University College London London UK

4. Department of Geography University of California Berkeley CA USA

Funder

Natural Environment Research Council

National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

Earth-Surface Processes,Geophysics

Reference117 articles.

1. Deformation of till beneath ice stream B, West Antarctica

2. Glacial erosion: status and outlook

3. Glaciological and geological implications of basal‐ice accretion in overdeepenings;Alley R. B.;Special Papers—Geological Society of America,1999

4. Discovery of Till Deposition at the Grounding Line of Whillans Ice Stream

5. Widespread erosion on high plateaus during recent glaciations in Scandinavia

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