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The polymorphism of sericite

Published online by Cambridge University Press:  14 March 2018

Mitsuoki Nakahira
Mitsuoki Nakahira*
Affiliation:
Scientific Research Institute, Kamifuge-Mae, Komagome, Bunkyo-Ku, Tokyo, Japan
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Abstract

A sericite from Unnan Mine, Shimane Prefecture, Japan, has a three-layer structure, perhaps similar to three-layer phlogopite and lepidolite, but with various degrees of disorder in inter-layer stacking, in different samples. A classification of polymorphic and disordered forms, showing their relationship, is proposed.

Type
Research Article
Information
Clay Minerals Bulletin , Volume 2 , Issue 12 , December 1954 , pp. 141 - 146
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1954

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References

Hendricks, S. B. and Jefferson, M. E., 1939. Amer. Min., 24, 729.Google Scholar
Minato, H. and Takano, Y., 1952. Sci. Pap. Coll. General Education Univ., Tokyo, 2, 189.Google Scholar
Nakahira, M., 1953. J. Sci. Research inst., 29, 446.(in Japanese). (Briefly in Acta Cryst. (1952), 5, 699).Google Scholar