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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.1960.032.249.02</article-id>
<title-group>
<article-title>X-ray Data on Stokesite</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Gay</surname>
<given-names>P.</given-names></name> <degrees>M.A., Ph.D.</degrees></contrib>
<contrib contrib-type="author">
<name>
<surname>Rickson</surname>
<given-names>K. O.</given-names>
</name></contrib>
<aff>Dept. of Mineralogy and Petrology, Downing Place, Cambridge</aff></contrib-group>
<pub-date pub-type="ppub">
<month>6</month>
<year>1960</year>
</pub-date>
<volume>32</volume>
<issue>249</issue>
<fpage>433</fpage>
<lpage>435</lpage>
<copyright-statement>Copyright &#x00A9; 1960, The Mineralogical Society</copyright-statement>
<copyright-year>1960</copyright-year>
<abstract>
<title>Summary</title>
<p>An X-ray examination of the type specimen of stokesite gave <italic>a</italic> 14&#x00B7;41, <italic>b</italic> 11&#x00B7;61, <italic>c</italic> 5&#x00B7;23 &#x00C5;.; space-group <italic>Pnna</italic>. The unit cell contains 4[CaSnSi<sub>3</sub>O<sub>11</sub>H<sub>4</sub>] and is derived from Hutchinson's morphological unit by the transformation [010/001/100]. X-ray powder data are given.</p></abstract>
</article-meta>
</front>
</article>
