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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.1963.033.261.06</article-id>
<title-group>
<article-title>Some Natural Analcime Solid Solutions</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Wilkinson</surname>
<given-names>J. F. G.</given-names>
</name><degrees>M.Sc., Ph.D.</degrees>
<aff>Department of Geology, The University of New England, Armidale, N.S.W.</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>6</month>
<year>1963</year>
</pub-date>
<volume>33</volume>
<issue>261</issue>
<fpage>498</fpage>
<lpage>505</lpage>
<copyright-statement>Copyright &#x00A9; 1963, The Mineralogical Society</copyright-statement>
<copyright-year>1963</copyright-year>
<abstract>
<title>Summary</title>
<p>Chemical, optical, and X-ray data are presented on three analcimes from a differentiation sequence, olivine-theralite to analcime-tinguaite; compared with the ideal analcime composition, they reveal replacement of NaAl&#x2192;Si. Optical and X-ray data on these minerals accord reasonably well with analcimes possessing similar compositions, and synthesized in the sub-solidus region in the NaAlSiO<sub>4</sub>-NaAlSi<sub>3</sub>O<sub>8</sub>-H<sub>2</sub>O system.</p></abstract>
</article-meta>
</front>
</article>
