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High-iron bustamite and fluorapatite from the Broken Hill mine, New South Wales, Australia

Published online by Cambridge University Press:  05 July 2018

K. Harada ,
H. Sekino ,
K. Nagashima ,
T. Watanabe  and
H. Momoi
K. Harada
Affiliation:
Department of Chemistry, Faculty of Science, Tokyo University of Education, Otsuka, Bunkyo, Tokyo II2
H. Sekino
Affiliation:
Department of Chemistry, Faculty of Science, Tokyo University of Education, Otsuka, Bunkyo, Tokyo II2
K. Nagashima
Affiliation:
Department of Chemistry, Faculty of Science, Tokyo University of Education, Otsuka, Bunkyo, Tokyo II2
T. Watanabe
Affiliation:
Department of Geology, Faculty of Science, Kyushu University, Fukuoka, Japan 812
H. Momoi
Affiliation:
Department of Geology, Faculty of Science, Kyushu University, Fukuoka, Japan 812
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Summary

High-iron bustamite and apatite occur as subhedral large crystals up to 1 to 2 cm wide and 10 cm long in close association with spessartine in the disseminated sphalerite- and galena-bearing diopside-roepperite-calcite skarn at the New Broken Hill Consolidated mine (N.B.H.S.), New South Wales, Australia. Complete chemical analyses of the minerals have been made, together with physical, optical, and X-ray studies.

Type
Research Article
Information
Mineralogical Magazine , Volume 39 , Issue 305 , March 1974 , pp. 601 - 604
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1974

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