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Victoria University Antarctic Research Expedition Science and Logistics Reports 2002-03: VUWAE 47

REFERENCES

REFERENCES

Bannister, S. and Naish, T.R. 2002. ANDRILL Site Investigations, New Harbour and McMurdo Ice Shelf, Southern McMurdo Sound, Antarctica. Institute of Geological and Nuclear Sciences Report 2002/01, 24 p.

Domack, E.W., Jacobson, E.A., Shipp, S. and Anderson, J.B. 1999. Late Pleistocene-Holocene retreat of the West Antarctic Ice Sheet system in the Ross Sea: Part 2 – sedimentologic and stratigraphic signature. Geological Soc. America Bull., 111, 1517-1536.

Horgan, H., Naish, T., Bannister, S., Balfour, N., Wilson, G., Finnemore, M. and Pyne, A. 2003. Seismic stratigraphy of the Ross Island flexural moat under the McMurdo-Ross Ice Shelf, Antarctica. Immediate Scientific Report to AntarcticaNZ

Jacobs, S.S., Fairbanks, R.G. and Horibe, Y., 1985. Origin and evolution of water masses near the Antarctic continental margin: evidence from H218O/H216O ratios in seawater, American Geophysical Union Antarctic Research Series, vol. 43, 59-85.

Joughin, I. and Tulaczyck, S. 2001. Positive mass balance of Ross Ice Streams, West Antarctica. Science, 295, 476-480

page 9

Kellogg, T.B., Hughes, T. and Kellogg, D.E. 1996. Late Pleistocene interactions of East and West Antarctic ice-flow regimes: evidence from the McMurdo Ice Shelf. Journal of Glaciology, 42, 486-499.

Lacy, L, Harwood, D. and Levy, R. (eds.), 2002. Future Antarctic Margin Drilling: Developing a Science Program Plan for McMurdo Sound. Andrill Contribution 1. University of Nebraska-Lincoln, Lincoln, NE xxx pp.

Meluish, A, Henrys, S.A., Bannister, S. and Davey, F.J., 1995. Seismic profiling adjacent to Ross Island: constraints on Late Cenozoic stratigraphy and tectonics. Terra Antartica, 2, 127-136.

Nixdorf, U., Oeter, H. and Miller, H., 1994. First access to the ocean beneath Ekströmisen, Antarctica, by means of hot-water drilling. Annals of Glaciology, 20, 110-114.

Fig. 6. Sediment deposited beneath the McMurdo Ice Shelf in the last 8000 years or so.

Fig. 6. Sediment deposited beneath the McMurdo Ice Shelf in the last 8000 years or so.