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Spilitic Rocks in New Zealand

Published online by Cambridge University Press:  01 May 2009

J. A. Bartrum
J. A. Bartrum
Affiliation:
Auckland University College, New Zealand.
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Extract

Prior to a discovery made recently by the writer, of spilitic rocks at Great King Island, the largest member of the Three Kings group of islands, about 26 miles north-west of the north-west extremity of the mainland of New Zealand, such rocks had not previously been found in this latter country. Some account of the types represented at Great King Island may therefore be welcome, particularly since Gilluly's (1935) recent comprehensive paper has focused attention on spilites and their associations.

Type
Original Articles
Information
Geological Magazine , Volume 73 , Issue 9 , September 1936 , pp. 414 - 423
Copyright
Copyright © Cambridge University Press 1936

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References

LITERATURE REFERRED TO

Bartrum, J. A., 1934. “The Pillow-lavas and Associated Rocks of North Cape Area, New Zealand,” N.Z. Journ. Sci. and Techn., xvi, 158–9.Google Scholar
Bartrum, J. A., 1935. “Metamorphic Rocks and Albite-rich Igneous Rocks from Jurassic Conglomerates at Kawhia,” Trans. Soy. Soc.N.Z., lxv, 95–107.Google Scholar
Bartrum, J. A., and Turner, F. J., 1928. “Pillow-lavas, Peridotites and Associated Rocks of Northermost New Zealand,” Trans. N.Z. Inst., lix, 98–138.Google Scholar
Bell, J. M., and Clarke, E. de c., 1909. “The Geology of the Whangaroa Subdivision,” N. Z. Geol. Surv. Bull., No. 8 (n.s.).Google Scholar
Gilluly, J., 1935. “Keratophyres of Eastern Oregon and the Spilite Problem,” Amer. Journ. Sci., ser. 5, xxix, 225–252 and 336–352.CrossRefGoogle Scholar
Sundius, N., 1930. “On the Spilitie Rocks,” Geol. Mag., lxvii, 1–17.CrossRefGoogle Scholar
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