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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.1960.032.248.06</article-id>
<title-group>
<article-title>Chemical Variations in Members of the Fergusonite-Formanite Series</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Butler</surname>
<given-names>J. R.</given-names>
</name><degrees>M.A., Ph.D.</degrees></contrib>
<contrib contrib-type="author">
<name>
<surname>Rosemary</surname>
<given-names>Hall</given-names>
</name></contrib>
<aff>Imperial College, South Kensington, London, S.W. 7.</aff></contrib-group>
<pub-date pub-type="ppub">
<month>3</month>
<year>1960</year>
</pub-date>
<volume>32</volume>
<issue>248</issue>
<fpage>392</fpage>
<lpage>407</lpage>
<copyright-statement>Copyright &#x00A9; 1960, The Mineralogical Society</copyright-statement>
<copyright-year>1960</copyright-year>
<abstract>
<title>Summary</title>
<p>Attention is drawn to anomalies in the nomenclature of the niobatetantalates, and the fergusonite series as used by Dana is renamed the fergusonite-formanite series. Chemical variations in this series are discussed with particular reference to H<sub>2</sub>O, Ca, Ti, Yt, individual lanthanons, Th, and U. Members of the series usually show heavy lanthanons exceeding light lanthanons but one specimen shows high Gd+Tb+Dy.</p></abstract>
</article-meta>
</front>
</article>
