Hostname: page-component-cd9895bd7-lnqnp Total loading time: 0 Render date: 2024-12-27T11:54:52.733Z Has data issue: false hasContentIssue false
  • English
  • Français

The kinetics of the low→high transformation in albite I. Amelia albite under dry conditions

Published online by Cambridge University Press:  14 March 2018

Duncan McKie  and
J. D. C. McConnell
Duncan McKie
Affiliation:
Department of Mineralogy and Petrology, Downing Place, Cambridge
J. D. C. McConnell
Affiliation:
Department of Mineralogy and Petrology, Downing Place, Cambridge
Get access Rights & Permissions [Opens in a new window]

Summary

The transformation was followed in Amelia albite powders by variation in 2θ131−2θ13̄1 with time under isothermal conditions at various temperatures in the range 920°–1080°C. The activation energy of about 74 kcal mole-1 is rather larger than that obtained for the ordering process in synthetic NaAlSi3O8 under hydrothermal conditions.

Type
Research Article
Information
Mineralogical magazine and journal of the Mineralogical Society , Volume 33 , Issue 262 , September 1963 , pp. 581 - 588
Copyright
Copyright © 1963, The Mineralogical Society

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

Fermuson, (R.B.), Traill, (R.J.), and Taylor, (W.H.), 1958.Acta Cryst., vol. I1, p. 331.CrossRefGoogle Scholar
Mcconnell, (J. D. C.), and Mckie, (D.), 1960.Min. Mag., vol.32, p. 436.Google Scholar
Mackenzie, (W.S.), 1957.Anler. Journ. Sci., vol.255, p. 481.Google Scholar
Pauling, (L.), 1960. The nature of the chemical bond. 3rd edn. Cornell University Press.Google Scholar
Schneider, (T.I.), 1957.Zeits. Krist., vol. 109, p. 245.Google Scholar
Tuttle, (O.F.) and Bowen, (N.L.), 1950.Journ. Geol., vol. 58, p. 572.Google Scholar