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Garnet-biotite relationships in high grade metamorphic rocks at Broken Hill, Australia

Published online by Cambridge University Press:  01 May 2009

I. R. Plimer
Affiliation:
The University of New South Wales, W.S. & L.B. Robinson University College, P.O. Box 334, Broken Hill, N.S.W., 2880Australia.

Summary

Garnets and biotites from pelitic, psammitic and quartzofeldspathic rock enclosing the Broken Hill orebodies are sensitive to syn and post high grade metamorphic metasomatism associated with orebody-wall rock reactions but the overall garnet—biotite partitioning relationships remain unchanged. KMg-FeDgarnet-biotite and metamorphic grade calculations increase from NW to SE over the 1000 m section examined which is in accord with the regional grade variation.

Type
Articles
Copyright
Copyright © Cambridge University Press 1976

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References

Albee, A. A. 1965. Distribution of Fe, Mg and Mn between garnet and biotite in natural mineral assemblages. J. Geol. 73, 155–64.CrossRefGoogle Scholar
Binns, R. A. 1964. Zones of progressive regional metamorphism in the Willyama Complex, Broken Hill district, New South Wales. J. geol. Soc. Aust. 11, 283330.CrossRefGoogle Scholar
Binns, R. A. 1968. Experimental studies of metamorphism at Broken Hill. In (Eds): Radmanovich, M. & Woodcock, J. T. Broken Hill Mines — 1968. Monograph 3, 199204, Aust. Inst. Min. Met., Melbourne.Google Scholar
Frost, M. J. 1962. Metamorphic grade and iron-magnesium distribution between coexisting garnet-biotite and garnet-hornblende. Geol. Mag. 99, 427–38.CrossRefGoogle Scholar
Harry, W. T. 1950. Aluminium replacing silicon in some silicate lattices. Mineralog. Mag. 29, 142–9.Google Scholar
Hewins, R. H., 1975. Pyroxene geothermometry of some granulite facies rocks. Contr. Mineral. Petrol. 50, 205–9.CrossRefGoogle Scholar
Jones, T. R. 1968. Garnet sandstone and garnet rims at orebody contacts, Broken Hill. In (Eds): Radmanovich, M. & Woodcock, J. T. Broken Hill Mines — 1968. Monograph 3, 171–8, Aust. Inst. Min. Met., Melbourne.Google Scholar
Katz, M. B. 1976. Broken Hill — a Precambrian hot spot? Precamb. Res. 3, 91106.CrossRefGoogle Scholar
Pidgeon, R. T. 1967. A rubidium-strontium geochronological study of the Willyama Complex, Broken Hill, Australia. J. Petrology 8, 283324.CrossRefGoogle Scholar
Plimer, I. R. 1975. A metamorphogenic alteration zone around the stratiform Broken Hill ore deposits, Australia. Geochem. J. 9, 211220.CrossRefGoogle Scholar
Reed, S. J. B. & Ware, N. G. 1973. Quantitative electron microprobe analysis using a Li-drifted silicon detector. X-ray Spect. 2, 6974.Google Scholar
Rutland, R. W. R. & Etheridge, M. A. 1975. Two high grade schistosites at Broken Hill and their relation to major and minor structures. J. geol. Soc. Aust. 22, 259–75.CrossRefGoogle Scholar
Shaw, S. E. 1968. Rb—Sr isotopic studies of the mine sequence rocks. In (Eds): Radmanovich, M. & Woodcock, J. T. Broken Hill Mines — 1968. Monograph 3, 185–98, Aust. Inst. Min. Met., Melbourne.Google Scholar