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A clay mineral from Stjernøy, North Norway

Published online by Cambridge University Press:  14 March 2018

D. A. Holdridge*
Affiliation:
British Ceramic Research Association, Stoke-on-Trent
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Abstract

A thin vein of a white powdery material situated in massive syenite was examined by various methods and found to consist of an association of a zeolite with calcium montmorillonite, which seems to have been formed by the slow but prolonged action of water on nepheline.

Type
Research Article
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1962

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References

Keeling, P. S., 1958. Clay Min. Bull., 3, 271.CrossRefGoogle Scholar
Kolzumi, M., 1953. Miner. J., Japan, 1, 36.CrossRefGoogle Scholar
Mackenzie, R. C., and Robertson, R. H. S., 1962. Aeta Univ. Carol., Geol., Suppl. No. 1, in press.Google Scholar
Morey, G. W., and Fournier, R. O., 1961. Amer. Min., 46, 688.Google Scholar
Ross, C. S., and Hendrjcks, S. B., 1945. Prof. Pap. U.S. Geol. Surv., No. 205-B p. 23.Google Scholar

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