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Högbomite of unusual composition from Reedy Creek, South Australia

Published online by Cambridge University Press:  05 July 2018

N. S. Mancktelow
N. S. Mancktelow*
Affiliation:
Department of Geology and Mineralogy, University of Adelaide, Adelaide 5000, Australia
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Abstract

Högbomite from Reedy Creek, South Australia, is of a composition outside the previously reported range. It contains less Ti and Mg and more Al and total Fe, with a total Fe/(total Fe + Mg) value between 0.69 and 0.72. The högbomite occurs in unusual cordieritesillimanite aggregates containing minor magnetite, ilmenite, hematite, corundum, and hercynite.

Type
Research Article
Information
Mineralogical Magazine , Volume 44 , Issue 333 , March 1981 , pp. 91 - 94
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1981

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Footnotes

1

Present address: Geologisches Institut, ETH-Zentrum, CH-8092 Zürich, Switzerland.

References

McKie, D. (1963). Mineral. Mag. 33, 563-80.Google Scholar
Mancktelow, N.S. (1979). Ph.D. thesis, University of Adelaide.Google Scholar
Moore, A.C. (1971). J. Geol. Soc. Aust. 17, 227-9.CrossRefGoogle Scholar
Nel, H.J. (1949). S. Air. Geol. Surv. Mem. 43, 1-7.Google Scholar
Sando, M. (1957). M.Sc. thesis, University of Adelaide. Teale, G.S. (1980). Mineral. Mag. 43, 575-7.Google Scholar
White, A.J.R. (1966). Chem. Geol. 1, 165-200.CrossRefGoogle Scholar
Whitehead, B.R. (1975). B.Sc. Hons. thesis, University of Adelaide.Google Scholar
Wilson, A.F. (1977). Mineral. Mag. 41, 337-40.CrossRefGoogle Scholar
Zakrzewski, M.A. (1977). Neues Jahrb. Mineral. Monatsh. 373-80.Google Scholar