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Aitken, A. R. A., Roberts, J. L., Ommen, T. D. van, Young, D. A., Golledge, N. R., Greenbaum, J. S., Blankenship, D. D., Siegert, M. J. (2016) Repeated large-scale retreat and advance of Totten Glacier indicated by inland bed erosion. Nature, 533 (7603). 385-389 doi:10.1038/nature17447

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Reference TypeJournal (article/letter/editorial)
TitleRepeated large-scale retreat and advance of Totten Glacier indicated by inland bed erosion
JournalNature
AuthorsAitken, A. R. A.Author
Roberts, J. L.Author
Ommen, T. D. vanAuthor
Young, D. A.Author
Golledge, N. R.Author
Greenbaum, J. S.Author
Blankenship, D. D.Author
Siegert, M. J.Author
Year2016 (May)Volume533
Issue7603
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1038/nature17447Search in ResearchGate
Generate Citation Formats
Mindat Ref. ID3020072Long-form Identifiermindat:1:5:3020072:6
GUID0
Full ReferenceAitken, A. R. A., Roberts, J. L., Ommen, T. D. van, Young, D. A., Golledge, N. R., Greenbaum, J. S., Blankenship, D. D., Siegert, M. J. (2016) Repeated large-scale retreat and advance of Totten Glacier indicated by inland bed erosion. Nature, 533 (7603). 385-389 doi:10.1038/nature17447
Plain TextAitken, A. R. A., Roberts, J. L., Ommen, T. D. van, Young, D. A., Golledge, N. R., Greenbaum, J. S., Blankenship, D. D., Siegert, M. J. (2016) Repeated large-scale retreat and advance of Totten Glacier indicated by inland bed erosion. Nature, 533 (7603). 385-389 doi:10.1038/nature17447
In(2016, May) Nature Vol. 533 (7603) Springer Science and Business Media LLC

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Maritati, A., Aitken, A. R. A., Young, D. A., Roberts, J. L., Blankenship, D. D., Siegert, M. J. (2016) The tectonic development and erosion of the Knox Subglacial Sedimentary Basin, East Antarctica. Geophysical Research Letters, 43 (20) 10 doi:10.1002/2016gl071063
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Roberts, J. L., Warner, R. C., Young, D., Wright, A., van Ommen, T. D., Blankenship, D. D., Siegert, M., Young, N. W., Tabacco, I. E., Forieri, A., Passerini, A., Zirizzotti, A., Frezzotti, M. (2011) Refined broad-scale sub-glacial morphology of Aurora Subglacial Basin, East Antarctica derived by an ice-dynamics-based interpolation scheme. The Cryosphere, 5 (3). 551-560 doi:10.5194/tc-5-551-2011
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