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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.1960.032.250.07</article-id>
<title-group>
<article-title>Magnetic Susceptibility of Garnet</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Frost</surname>
<given-names>M. J.</given-names>
</name><degrees>B.Sc., Ph.D., F.G.S.</degrees>
<xref ref-type="author-notes" rid="FN1">1</xref>
<aff>Department of Geology, University of Western Australia.</aff></contrib></contrib-group>
<author-notes>
<fn fn-type="present-address" id="FN1"><label>1</label><p>Pressent address: Department of Geology, The University of Canterbury, Christchurch, C.l, New Zealand.</p></fn></author-notes>
<pub-date pub-type="ppub">
<month>9</month>
<year>1960</year>
</pub-date>
<volume>32</volume>
<issue>250</issue>
<fpage>573</fpage>
<lpage>576</lpage>
<copyright-statement>Copyright &#x00A9; 1960, The Mineralogical Society</copyright-statement>
<copyright-year>1960</copyright-year>
<abstract>
<title>Summary</title>
<p>The mass suseeptibility of 23 analysed or partially analysed garnets has been measured by means of a calibrated Franz Isodynamic magnetic separator. Straight lines are fitted to the adjusted data for mass susceptibility and molecular composition. The mass susceptibilities of the theoretical end-members in electromagnetic units &#x00D7; 10<sup>6</sup> are estimated as: almandine, 68&#x00B1;2 e.m.u.; spessartine, 81&#x00B1;3 e.m.u.; and andradite, 49&#x00B1;3 e.m.u. Grossular and pyrope are assumed to have susceptibilities of nil.</p></abstract>
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</front>
</article>
