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<article article-type="research-article">
<front>
<journal-meta>
<journal-id journal-id-type="archive">gsminmag</journal-id>
<journal-title>Mineralogical Magazine</journal-title>
<abbrev-journal-title abbrev-type="full">Mineralogical Magazine</abbrev-journal-title>
<issn pub-type="ppub">0026-461X</issn>
<publisher>
<publisher-name>Mineralogical Society</publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.1180/minmag.1978.042.321.11</article-id>
<title-group>
<article-title>Manganoan Ilvaite from Broken Hill, N.S.W. Ban Ban, Queensland, Australia</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Plimer</surname>
<given-names>I. R.</given-names>
</name>
<aff>University of New South Wales, P.O. Box 334, Broken Hill, N.S.W. 2880</aff></contrib>
<contrib contrib-type="author">
<name>
<surname>Ashley</surname>
<given-names>P. M.</given-names>
</name>
<aff>Minerals Department, Esso Australia Ltd., G.P.O. Box 4047, Sydney, N.S.W. 2001</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>3</month>
<year>1978</year>
</pub-date>
<volume>42</volume>
<issue>321</issue>
<fpage>85</fpage>
<lpage>88</lpage>
<history>
<date date-type="received">
<day>16</day>
<month>5</month>
<year>1977</year>
</date>
<date date-type="rev-recd">
<day>1</day>
<month>8</month>
<year>1977</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1978, The Mineralogical Society</copyright-statement>
<copyright-year>1978</copyright-year>
<abstract>
<title>Summary</title>
<p>Manganoan ilvaite forms as an early retrograde metamorphic phase from calcic rhodonite in the polymetamorphosed Pb-Zn sulphide/manganese silicate rocks at Broken Hill and from grossular-andradite in a skarn at Ban Ban. Ilvaite exists as a probable metastable phase into which Mn is apparently strongly partitioned. The manganoan ilvaites analysed contain up to 13&#x00B7;5 % MnO substituting for FeO and this substitution shifts the 020 peak.</p></abstract>
</article-meta>
</front>
</article>
