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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.1998.62A.3.135</article-id>
<title-group>
<article-title>Adam-Gibbs Theory and the Prediction of Glass Transition Temperatures: The Join Na<sub>2</sub>Si<sub>2</sub>O<sub>5</sub>-NaAlSi<sub>2</sub>O<sub>6</sub></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Toplis</surname>
<given-names>M. J.</given-names>
</name>
<aff>CRPG-CNRS, Vandoeuvre-l&#x00E8;s-Nancy, F-54501, France</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<year>1998</year>
</pub-date>
<volume>62A</volume>
<issue>3</issue>
<fpage>1527</fpage>
<lpage>1528</lpage>
<copyright-statement>Copyright &#x00A9; 1998, The Mineralogical Society</copyright-statement>
<copyright-year>1998</copyright-year>
</article-meta>
</front>
</article>
