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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.1968.036.282.04</article-id>
<title-group>
<article-title>The Role of Titanium and the Effect of TiO<sub>2</sub> on the Cell-Size, Refractive Index, and Specific Gravity in the Andradite-Melanite- Schorlomite Series</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Howie</surname>
<given-names>R. A.</given-names>
</name>
<aff>Department of Geology, King's College, London, W.C.2</aff></contrib>
<contrib contrib-type="author">
<name>
<surname>Woolley</surname>
<given-names>A. R.</given-names>
</name>
<aff>Department of Mineralogy, British Museum (Natural History), Cromwell Road, London, S.W. 7</aff></contrib></contrib-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Scoon</surname>
<given-names>J. H.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Tyler</surname>
<given-names>R. C.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Walsk</surname>
<given-names>J. N.</given-names>
</name></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>6</month>
<year>1968</year>
</pub-date>
<volume>36</volume>
<issue>282</issue>
<fpage>775</fpage>
<lpage>790</lpage>
<history>
<date date-type="received">
<day>18</day>
<month>12</month>
<year>1957</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1968, The Mineralogical Society</copyright-statement>
<copyright-year>1968</copyright-year>
<abstract>
<title>Summary</title>
<p>New chemical analyses, cell-sizes, and specific gravities are given for 12 garnets, and TiO<sub>2</sub> values, cell-sizes, and refractive indices are presented for a further 33 garnets all belonging to the andradite-melanite-schorlomite series. The increase of refractive index, cell-size, and specific gravity with increasing titania is shown graphically. A plot of Ti against Si atoms in the unit cell suggests that Ti replaces Si rather than Fe<sup>3+</sup> in the structure, while electron-probe results indicate that Si or (Si+Fe) may be replaced by Ti. The chemical and infra-red absorption data are considered in a discussion of the structural role of titanium in these garnets : both Ti<sup>4+</sup> and Ti<sup>3+</sup> may be present.</p></abstract>
</article-meta>
</front>
</article>
