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Corona structures formed by near-isochemical reaction between olivine and plagioclase in a metamorphosed dolerite

Published online by Cambridge University Press:  05 July 2018

R. N. England
R. N. England*
Affiliation:
Bureau of Mineral Resources Canberra, Australia
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Abstract

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Type
Short Communications
Information
Mineralogical Magazine , Volume 39 , Issue 307 , September 1974 , pp. 816 - 818
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1974

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Footnotes

1

Published with permission of the Director, Bureau of Mineral Resources, Canberra, A.C.T., Australia.

References

Griffin, (W. L.), 1971. Journ. Petrology, 12,219.CrossRefGoogle Scholar
Mason, (R.), 1967. Min. Mag., 36, 504.Google Scholar
Murthy, (M. V. N.), 1958. Bull. Geol. Soc. Amer., 69, 23.CrossRefGoogle Scholar
Robie, (R. A.), Bethke, (D. M.), and Beardsley, (K. M.), 1967. U.S. Geol. Surv. Bull., 1248.Google Scholar
Whitney, (P. R.) and Mclelland, (J. M.), 1973. Contr. Min. Petr., 39, 81–98.CrossRefGoogle Scholar