Cosmogenic nuclides Be-10 and Al-26 imply limited Antarctic Ice Sheet thickening and low erosion in the Shackleton Range for > 1 m.y.
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Date
2004-03Type
- Journal Article
ETH Bibliography
yes
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Publication status
publishedExternal links
Journal / series
GeologyVolume
Pages / Article No.
Publisher
Geological Society of AmericaSubject
Shackleton Range; Cosmogenic isotopes; Geomorphology; Ice-sheet change; Erosion ratesMore
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ETH Bibliography
yes
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