Hostname: page-component-5c6d5d7d68-qks25 Total loading time: 0 Render date: 2024-08-16T02:24:18.676Z Has data issue: false hasContentIssue false
  • English
  • Français

Co-Existing Pyroxenes

Published online by Cambridge University Press:  01 May 2009

P. E. Brown
P. E. Brown
Affiliation:
Department of Geology, Sheffield.
Rights & Permissions [Opens in a new window]

Abstract

An abstract is not available for this content so a preview has been provided. As you have access to this content, a full PDF is available via the ‘Save PDF’ action button.
Image of the first page of this content. For PDF version, please use the ‘Save PDF’ preceeding this image.'
Type
Correspondence
Information
Geological Magazine , Volume 98 , Issue 6 , December 1961 , pp. 531 - 535
Copyright
Copyright © Cambridge University Press 1961

References

REFERENCES

Brown, G. M., 1957. Pyroxenes from the early and middle stages of fractionation of the Skaergaard intrusion. Miner. Mag., 31, 511–543.Google Scholar
De Vore, G. W., 1957. The association of strongly polarizing cations with weakly polarizing cations as a major influence in element distribution, mineral composition, and crystal growth. J. Geol., 65, 178–195.Google Scholar
Kretz, R., 1959. Chemical study of garnet, biotite, and hornblende from gneisses of south-western Quebec, with emphasis on distribution of elements in co-existing minerals. J. Geol., 67, 371–402.Google Scholar
Kretz, R., 1961. Some applications of thermodynamics to co-existing minerals of variable compositions. Examples: Orthopyroxene-clinopyroxene and orthopyroxene-garnet. J. Geol., 69, 361–387.Google Scholar
Ramberg, H., and De Vore, G. W., 1951. The distribution of Fe++ and Mg++ in co-existing olivines and pyroxenes. J. Geol., 59, 193–210.Google Scholar
Wager, L. R., 1960. The relationship between fractionation stage of basalt magma and the temperature of the beginning of its crystallization. Genchim. et Cosmnrhim. Acta. 20. 158–160.CrossRefGoogle Scholar