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Non–Equivalence of Distribution Coefficients and Tie–lines of Coecisting Pyroxenes

Published online by Cambridge University Press:  01 May 2009

M. J O'Hara
Affiliation:
Grant Institute of Geology, West Mains Road, Edinburgh, 9.
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Abstract

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Type
Correspondence
Copyright
Copyright © Cambridge University Press 1964

References

REFERENCES

Bartholomè, P., 1961. Coexisting pyroxenes in igneous and metamorphic rocks. Geol. Mag., 98, 346348.CrossRefGoogle Scholar
Collee, A. L. G., 1962. A fabric study of lherzolites. Leidse. Geol. Meded., 28, 1102.Google Scholar
Kretz, R., 1961. Some applications of thermodynamics to coexisting minerals of variable composition. Examples: orthopyroxene–clinopyroxene and orthopyroxene–garnet. J. Geol., 69, 361387.CrossRefGoogle Scholar
O'Hara, M. J., and Mercy, E. L. P., 1963. Petrology and petrogenesis of some garnetiferous peridotites. Trans. roy. Soc. Edinb., 65, 251314.CrossRefGoogle Scholar
Oosterom, M. G., 1962. The ultramafites and layered gabbro sequences in the granulite facies rocks on Stjernoy (Finnmark, Norway). Leidse. Geol. Meded., 28, 177296.Google Scholar