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Paragenesis of the Minerals of the Three Component System MgO-Al2O3-SiO2 in Thermal Metamorphism

Published online by Cambridge University Press:  01 May 2009

C. E. Tilley
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Extract

The system magnesia-alumina-silica is one of great importance in petrology, and the paragenesis of its constituent minerals must be a subject of study in any enquiry into the thermal metamorphism of rocks which have these three components as important constituents. Such rocks include particularly those of argillaceous type, magnesian-carbonate sediments, and bauxitic rocks.

Type
Research Article
Information
Geological Magazine , Volume 60 , Issue 3 , March 1923 , pp. 101 - 107
Copyright
Copyright © Cambridge University Press 1923

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References

page 102 note 1 The Ternary system MgO-Al2O3-SiO2, Rankin, G. A. and Merwin, H. E., Amer. Journ. Sci., vol. xlv, 1918, p. 301.CrossRefGoogle Scholar