Hostname: page-component-78c5997874-mlc7c Total loading time: 0 Render date: 2024-11-08T03:31:19.931Z Has data issue: false hasContentIssue false
  • English
  • Français

Clay mineralogical aspects of the alteration of volcanic glass in Japan

Published online by Cambridge University Press:  14 March 2018

Toshio Sudo
Toshio Sudo*
Affiliation:
Geological and Mineralogical Institute, Faculty of Science, Tokyo University of Education, Otsukakubo-machi, Bunkyo-ku, Tokyo, Japan
Get access

Extract

The Japanese archipelago, in the temperate zone, has been affected by volcanic and hot spring action in many geological periods including the Recent one. Complicated clay mineral assemblages have been formed by alteration of volcanic glass both by weathering and hydrothermally, and have been studied by the writer and his collaborators (Sudo, 1950b, 1951; Sudo, Minato and Nagasawa, 1951; Sudo and Ossaka, 1952). The present account, based on these studies and on more recent data, deals with acidic to intermediate types of volcanic glass, which are widely distributed in rocks and soils throughout the islands.

Type
Research Article
Information
Clay Minerals Bulletin , Volume 2 , Issue 11 , May 1954 , pp. 96 - 106
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.)

References

Allaway, W. H., 1948. Differential thermal analysis of clays treated with organic cations as an aid in the study of soil colloids. Proc. Soil Sci. Soc. Amer., 13, 183–188.Google Scholar
Sudo, T., 1950a. Mineralogical notes of some opal and cristobalite. J. Geol. Soc. Japan, 56, 137–142.CrossRefGoogle Scholar
Sudo, T., 1950b. Mineralogical studies of zeolite-bearing pumice tuff near Yokote-machi, Akita Prefecture. Ibid. 56, 13–16.Google Scholar
Sudo, T., 1950c. Iron-montmorillonite from the Hanaoka Mine, Akita Prefecture. Proc. Imp. Acad. Japan, 26, 91–95.CrossRefGoogle Scholar
Sudo, T., 1951. Mineralogy of green tuff breccia near Shiroishimachi, Miyagi Prefecture. J. Geol. Soc. Japan, 57, 347–355.Google Scholar
Sudo, T., Minato, H. and Nagasawa, K., 1951. J. Geol. Soc. Japan, 57, 473–480.CrossRefGoogle Scholar
Sudo, T. and Nakamura, T., 1952. Hisingerite from Japan. Amer. Min., 37, 618–621.Google Scholar
Sudo, T. and Ota, S., 1952. An iron-rich variety of montmorillonite found in Oya-ishi. J. Geol. Soc. Japan, 58, 487–491.CrossRefGoogle Scholar
Sudo, T. and Ossaka, J., 1952. Hydrated halloysite from Japan. Jap. J. Geol. Geogr., 22, 215–229.Google Scholar