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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.1984.048.348.13</article-id>
<title-group>
<article-title>Gahnite Compositions Compared</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Batchelor</surname>
<given-names>Richard A.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Kinnaird</surname>
<given-names>Judith A.</given-names>
</name></contrib>
<aff>Department of Geology, University of St Andrews, St Andrews, Fife, Scotland</aff></contrib-group>
<pub-date pub-type="ppub">
<month>9</month>
<year>1984</year>
</pub-date>
<volume>48</volume>
<issue>348</issue>
<fpage>425</fpage>
<lpage>429</lpage>
<history>
<date date-type="received">
<day>9</day>
<month>9</month>
<year>1983</year>
</date>
<date date-type="rev-recd">
<day>25</day>
<month>11</month>
<year>1983</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1984, The Mineralogical Society</copyright-statement>
<copyright-year>1984</copyright-year>
<abstract>
<title>Abstract</title>
<p>Blue-coloured gem-quality spinel from Nigeria was analysed by wet chemical methods (using atomic absorption spectrophotometry) and investigated by X-ray diffraction. The results showed it to be gahnite (unit cell dimension <italic>a</italic>=8.091&#x00B1;0.003 &#x00C5;) containing 36.7% ZnO, 3.58% FeO, and 0.12% MgO. The spinel has an RI of 1.79 and density between 4.4 and 4.59. Broadening of the <italic>n</italic>[111] XRD reflections indicates a measure of compositional heterogeneity. The gahnite analyses were compared with compositions of zinc spinels from other parts of the world. The analyses cluster into two distinct groups, Mg-rich spinels of metamorphic origin and Mg-poor spinels (including the Nigerian gahnite) with igneous affinities. Diadochy seems to operate within the zinc spinel structure between (Zn + Mn) and (Fe + Mg).</p></abstract>
</article-meta>
</front>
</article>
