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<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.1974.039.306.09</article-id>
<title-group>
<article-title>An E.S.R. Study of Natural Fluorite Containing Manganese Impurities</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Bailey</surname>
<given-names>A. D.</given-names>
</name>
<xref ref-type="author-notes" rid="FN1">1</xref></contrib>
<contrib contrib-type="author">
<name>
<surname>Hunt</surname>
<given-names>R. P.</given-names>
</name>
<xref ref-type="author-notes" rid="FN2">2</xref></contrib>
<contrib contrib-type="author">
<name>
<surname>Taylor</surname>
<given-names>K. N. R.</given-names>
</name>
<xref ref-type="author-notes" rid="FN3">3</xref></contrib></contrib-group>
<author-notes>
<fn fn-type="present-address" id="FN1"><label>1</label><p>Now at University of Bath, England.</p></fn>
<fn fn-type="present-address" id="FN2"><label>2</label><p>Now at CEGB Nuclear Research Laboratory, Berkeley, England.</p></fn>
<fn fn-type="present-address" id="FN3"><label>3</label><p>Now at Physics Dept. University of N.S.W. Sydney, Australia.</p></fn></author-notes>
<pub-date pub-type="ppub">
<month>6</month>
<year>1974</year>
</pub-date>
<volume>39</volume>
<issue>306</issue>
<fpage>705</fpage>
<lpage>708</lpage>
<history>
<date date-type="received">
<day>10</day>
<month>4</month>
<year>1973</year>
</date>
<date date-type="rev-recd">
<day>10</day>
<month>10</month>
<year>1973</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1974, The Mineralogical Society</copyright-statement>
<copyright-year>1974</copyright-year>
<abstract>
<title>Summary</title>
<p>The electron spin resonance spectrum of a sample of natural, orange-coloured fluorite from Broken Hill, Australia, has been observed and shown to arise from the presence of manganese ions. From an analysis of the structure of this spectrum it has been possible to estimate the various contributions to the ionic energy level splitting and to show that these are in good agreement with comparable results for synthetic material. It is evident that the manganese ions have entered the lattice substitutionally at Ca<sup>2+</sup> sites and the nature of this site is discussed.</p></abstract>
</article-meta>
</front>
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