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An Experimental Synthesis of Quartz, Albite, and Analcite

Published online by Cambridge University Press:  01 May 2009

Gilbert Wilson
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Abstract

Quartz sand, sodium aluminate and water were heated together in a bomb to above the critical temperature. The apparatus was designed to give a temperature difference of about 100°C. between the two ends of the bomb. Quartz, albite, and analcite were formed in the low temperature end of the bomb.

Type
Articles
Information
Geological Magazine , Volume 87 , Issue 1 , February 1950 , pp. 41 - 44
Copyright
Copyright © Cambridge University Press 1950

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References

1 MacGregor, M., and Wilson, G., 1939. On granitization and associated processes. Geol. Mag., lxxvi, 193.CrossRefGoogle Scholar

2 Perrin, R., and Roubault, M., 1937. Les réactions à l' état solide et la géologie. Bull. Serv. Carte géol. Algérie. Sér. 5, Pétrographie No. 1.Google Scholar Perrin, R., and Roubault, M., 1939. Le granite et les réactions a l'état solide. Bull. Serv. Carte géol. Algérie. Sér. 5, Pétrographie, No. 4.Google Scholar Bugge, J. A. W., 1946. The geological importance of diffusion in the solid state. Skrifter Norske Videnskaps-Akad. Oslo. I. Mat-Nature Kl. 1945, No. 13.Google Scholar