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Cosmogenic nuclides Be and Al imply limited Antarctic Ice Sheet thickening and low erosion in the Shackleton Range for > 1 m.y.

Fogwill, C.J.; Bentley, M.J.; Sugden, D.E.; Kerr, A.R.; Kubik, P.W.

Authors

C.J. Fogwill

D.E. Sugden

A.R. Kerr

P.W. Kubik



Citation

Fogwill, C., Bentley, M., Sugden, D., Kerr, A., & Kubik, P. (2004). Cosmogenic nuclides Be and Al imply limited Antarctic Ice Sheet thickening and low erosion in the Shackleton Range for > 1 m.y. Geology, 32(3), 265-268. https://doi.org/10.1130/g19795.1

Journal Article Type Article
Publication Date 2004
Journal Geology
Print ISSN 0091-7613
Electronic ISSN 1943-2682
Publisher Geological Society of America
Volume 32
Issue 3
Pages 265-268
DOI https://doi.org/10.1130/g19795.1
Public URL https://durham-repository.worktribe.com/output/1597682