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Kornerupiue in metasomatic zones, Strangways Range, Central Australia

Published online by Cambridge University Press:  05 July 2018

P. J. Woodford  and
Allan F. Wilson
P. J. Woodford
Affiliation:
Department of Geology and Mineralogy, University of Queensland, Australia, 4067
Allan F. Wilson
Affiliation:
Department of Geology and Mineralogy, University of Queensland, Australia, 4067
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Summary

The first known occurrence of kornerupine in Australia is described. The mineral is a minor component of a phlogopite-rich garnet-corundum-spinel metasomatic zone, which cuts mafic and ultranlafic spinel-plagioclase-orthopyroxene-hornblende rocks. The kornerupine-bearing assemblage was formed during the second major metamorphic episode that affected the terrain, probably under low-grade granulite or upper amphibolite facies conditions. Kornerupine appears to have formed at significantly lower levels of P-T than those reached in the terrain during the peak of the second granulite metamorphism.

Information

Type
Research Article
Information
Mineralogical Magazine , Volume 40 , Issue 314 , June 1976 , pp. 589 - 594
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1976

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