Research Collection Journal Article Dating late Cenozoic erosional surfaces in Victoria Land, Antarctica, with cosmogenic neon in pyroxenes Author(s): Oberholzer, P.; Baroni, C.; Salvatore, M. C.; Baur, H.; Wieler, R. Publication Date: 2008 Permanent Link: https://doi.org/10.3929/ethz-b-000010464 Originally published in: Antarctic Science 20(1), http://doi.org/10.1017/S095410200700079X Rights / License: In Copyright - Non-Commercial Use Permitted This page was generated automatically upon download from the ETH Zurich Research Collection. For more information please consult the Terms of use. ETH Library Antarctic Science 20 (1), 89–98 (2008) & Antarctic Science Ltd 2008 Printed in the UK DOI: 10.1017/S095410200700079X Dating late Cenozoic erosional surfaces in Victoria Land, Antarctica, with cosmogenic neon in pyroxenes P. OBERHOLZER1*, C. BARONI2, M.C. SALVATORE3, H. BAUR1 and R. WIELER1 1Institute of Isotope Geology and Mineral Resources, ETH Zu¨rich, Clausiusstrasse 25, 8092 Zu¨rich, Switzerland 2Dipartimento di Scienze della Terra, Universita` di Pisa, Via S. Maria 53, 56126 Pisa, Italy 3Dipartimento di Scienze della Terra, Universita` di Roma “La Sapienza”, Piazzale A. Moro 5, 00185 Roma, Italy *current address: Baugeologie und Geo-Bau-Labor Chur, Bolettastrasse 1, 7000 Chur, Switzerland
[email protected] Abstract: We present 21Ne exposure ages of erosional glaciogenic rock surfaces on nunataks in northern Victoria Land, Antarctica: i) in the Prince Albert Mountains and ii) near Mesa Range. These nunataks are located directly at the margin of the polar plateau and therefore provide an immediate record of ice volume changes of the East Antarctic Ice Sheet, not biased by ice shelf grounding or narrow valley sections downstream the outlet glaciers.