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The Influence of Ionic Substitution on the Hydrothermal Stability of Montmorillonoids

Published online by Cambridge University Press:  01 January 2024

F. A. Mumpton  and
Rustum Roy
F. A. Mumpton
Affiliation:
The Pennsylvania State University, University Park, Pennsylvania, USA
Rustum Roy
Affiliation:
The Pennsylvania State University, University Park, Pennsylvania, USA
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Abstract

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Type
Article
Information
Clays and Clay Minerals (National Conference on Clays and Clay Minerals) , Volume 4 , February 1955 , pp. 337 - 339
Copyright
Copyright © The Clay Minerals Society 1955

Footnotes

Contribution No. 55–28, The College of Mineral Industries, The Pennsylvania State University. Full paper to be published elsewhere.

References

Romo, L. A., and Roy, Rustum, 1955, Essais de synthèse des minéraux argileux dits à “couches mixtes”: Bull. Soc. Franc. Miner. Crist., v. 78, p. 438–448.Google Scholar
Ross, C. S., 1946, Sauconite—a clay mineral of the montmorillonite group: Amer. Min., v. 31, p. 411–424.Google Scholar
Roy, D. M., 1952, Phase equilibrium in the system MgO-Al2O3-H2O and the influence of SiO2, CO3 and N2O5 upon it: Ph.D. dissertation, The Pennsylvania State University.Google Scholar
Roy, Rustum, and Osborn, E. F., 1952, Some simple aids in the hydrothermal investigation of mineral systems: Econ. Geol., v. 47, p. 717–721.CrossRefGoogle Scholar
Roy, D. M., and Roy, Rustum, 1955, Synthesis and stability of minerals in the system MgO- Al2O3-SiO2-H2O: Amer. Min., v. 40, p. 147–178.Google Scholar
Yoder, H. S., 1952, The MgO-Al2O3-SiO2-H2O system and the related metamorphic facies: Amer. J. Sci., Bowen vol. 40 p. 569–627.Google Scholar