Hostname: page-component-586b7cd67f-t7fkt Total loading time: 0 Render date: 2024-11-28T13:57:14.969Z Has data issue: false hasContentIssue false
  • English
  • Français

Some interstratified clay minerals of the Taro valley

Published online by Cambridge University Press:  14 March 2018

Andrea Alietti
Andrea Alietti*
Affiliation:
Mineralogy Department, University of Modena, Italy
Get access

Abstract

The ophiolitic rocks appearing near Monte Chiaro, characterized by serpentine masses crossed by veins of talc, sometimes of remarkable thickness, are to be found on the right of the Taro river a few miles from Borgotaro. On examination three interstratified clay minerals were found: saponite-talc, chlorite-saponite, chlorite-vermiculite, which were studied optically, with X-ray, d.t.a. and chemical analysis.

Type
Research Article
Information
Clay Minerals Bulletin , Volume 3 , Issue 19 , August 1958 , pp. 207 - 211
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1958

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

Mackenzie, R. C. 1957. The differential thermal investigation of clays. Mineralogical Society, London.Google Scholar