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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
Affiliation:
Department of Mineralogy and Petrology, Downing Place, Cambridge
J. D. C. McConnell
Affiliation:
Department of Mineralogy and Petrology, Downing Place, Cambridge

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
Copyright
Copyright © 1963, The Mineralogical Society

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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