Hostname: page-component-784d4fb959-wxg6b Total loading time: 0 Render date: 2025-07-14T20:43:56.560Z Has data issue: false hasContentIssue false
  • English
  • Français

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
Get access

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.

Information

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

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

Article purchase

Temporarily unavailable

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