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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.1958.031.242.06</article-id>
<title-group>
<article-title>Heat Treatment of Metamict Euxenites, Polymignites, Yttrotantalites, Samarskites, Pyrochlores, and Allanites</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Lima-de-Faria</surname>
<given-names>J.</given-names>
</name>
<aff>Mineralogical Museum, Section of the Junta de Investiga&#x00E7;&#x00F5;es do Ultramar, Faculty of Science, Lisbon, Portugal.</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>9</month>
<year>1958</year>
</pub-date>
<volume>31</volume>
<issue>242</issue>
<fpage>937</fpage>
<lpage>942</lpage>
<copyright-statement>Copyright &#x00A9; 1958, The Mineralogical Society</copyright-statement>
<copyright-year>1958</copyright-year>
<abstract>
<title>Summary</title>
<p>The standard thermal treatments proposed by Lima-de-Faria have been applied to metamict euxenites, polymignites, yttrotantalites, samarskites, pyrochlores, and allanites. In the case of these metamict niobotantalates a facecentred cubic phase is formed at 700&#x00B0; C., and at 1000&#x00B0;C. a more characteristic phase appears combined with the cubic one. In the case of allanites only a slight formation or strengthening of the original structure of allanite appears at 700&#x00B0;C., and at 1000&#x00B0;C. a cubic phase is formed together with other phases.</p></abstract>
</article-meta>
</front>
</article>
