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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.1983.047.343.11</article-id>
<title-group>
<article-title>A M&#x00F6;ssbauer Study of Some Australian Iron Ore Minerals</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Fysh</surname>
<given-names>S. A.</given-names>
</name>
<xref ref-type="author-notes" rid="FN1">*</xref>
<aff>Monash University, Clayton, Australia</aff></contrib>
<contrib contrib-type="author">
<name>
<surname>Ostwald</surname>
<given-names>J.</given-names></name>
<aff>The Broken Hill Proprietary Company Limited, Central Research Laboratories, Shortland, NSW, Australia, 2307</aff></contrib></contrib-group>
<author-notes>
<fn fn-type="current-aff" id="FN1"><label>*</label><p>Now at The Broken Hill Proprietary Company Limited, Central Research Laboratories, Shortland, NSW, Australia, 2307.</p></fn></author-notes>
<pub-date pub-type="ppub">
<month>6</month>
<year>1983</year>
</pub-date>
<volume>47</volume>
<issue>343</issue>
<fpage>209</fpage>
<lpage>217</lpage>
<history>
<date date-type="received">
<day>6</day>
<month>4</month>
<year>1982</year>
</date>
<date date-type="rev-recd">
<day>27</day>
<month>9</month>
<year>1982</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1983, The Mineralogical Society</copyright-statement>
<copyright-year>1983</copyright-year>
<abstract>
<title>Abstract</title>
<p>Six specimens of Australian iron ore, three hematite-rich and three goethite-rich, have been investigated by M&#x00F6;ssbauer spectroscopy at both 300 K and 4.2 K. The resulting spectra provide data relevant to crystallite particle size variations in the hematite and goethite, the extent of isomorphous replacement, and the existence within one specimen of a poorly defined goethite-like material.</p></abstract>
</article-meta>
</front>
</article>
