Hostname: page-component-cd9895bd7-jn8rn Total loading time: 0 Render date: 2025-01-06T01:20:22.051Z Has data issue: false hasContentIssue false
  • English
  • Français

Low-temperature thermal effects in natural volcanic glasses due to strain

Published online by Cambridge University Press:  14 March 2018

A. Ewart  and
M. Fieldes
A. Ewart
Affiliation:
New Zealand Geological Survey
M. Fieldes
Affiliation:
Soil Bureau, Department of Scientific and Industrial Research, New Zealand
Get access Rights & Permissions [Opens in a new window]

Summary

Sharp exothermic peaks occurring at about 90° C during D.T.A. treatment of natural volcanic glasses are described and are shown to be due to release of external strain. This is probably triggered by loss of surface water. No systematic variation in strain could be found in glass of different geological histories, but strain is found to decrease during natural weathering of volcanic glasses. Differences in weatherability of natural glasses may be related to degree of surface strain.

Type
Research Article
Information
Mineralogical magazine and journal of the Mineralogical Society , Volume 33 , Issue 258 , September 1962 , pp. 237 - 246
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1962

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

Baumgart, (I.L.), 1954. New Zealand Journ. Sci. Tech., vol. B35, p. 456.Google Scholar
Berkelhamer, (L.H.), 1944. U.S. Bureau of Mines Report of Investigations 3762.Google Scholar
Healy, (J.), 1962. Stratigraphy and Chronology of the Taupo and Rotorua Volcanic Ash. New Zealand Geol. Surv. Bull. 73.Google Scholar
Ross, (C.S.) and Smith, (R.L.), 1955. Amer. Min., vol. 40, p. 1071.Google Scholar