Abstract
THE Vestfold Hills, one of the so-called Antarctic oases, make up an area of exposed rock on the coast of Princess Elizabeth Land, Antarctica. The hills, together with the numerous adjacent islands, form a triangular area about 30 km across. The Australian National Antarctic Research Expedition (ANARE) station Davis is situated in the south-west of the hills at lat. 68° 35′ S., long. 77° 58′ E.
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McLeod, I. R., Trail, D. S., Cook, P. J., and Wallis, G. R., Bur. Min. Res. Austral. Rec. 1966/9 (unpublished).
Ravich, M. G., Sci. Res. Inst. Arctic Geol., 113, 25 (1960) (translation).
McCarthy, W. R., Austral. Min. Devel. Lab. Rep., MP, 604–65 (unpublished).
McCarthy, W. R., Austral. Min. Devel. Lab. Rep. MP, 1650–65 (unpublished).
Ravich, M. G., and Krylov, A. J., in Antarctic Geology (edit. by Adie, R. J.), 579 (North-Holland, Amsterdam, 1964).
McIntyre, G. A., Brooks, C., Compston, W., and Turek, A., J. Geophys. Res., 71, 5459 (1966).
Picciotto, E., and Coppez, A., Ann. Soc. Geol. Belg., 85, B263 (1963).
Webb, P. N., N.Z. J. Geol. Geophys., 5, 790 (1962).
Webb, P. N., and Warren, G., N.Z. J. Geol. Geophys., 8, 221 (1965).
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HARDING, R., MCLEOD, I. Age of Dolerite Dykes in the Vestfold Hills, Antarctica. Nature 215, 149–150 (1967). https://doi.org/10.1038/215149a0
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DOI: https://doi.org/10.1038/215149a0
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