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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.1956.031.235.08</article-id>
<title-group>
<article-title>Sepiolite at a Locality in the Keuper Marl of the Midlands</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Keeling</surname>
<given-names>P. S.</given-names>
</name> <degrees>B.Sc., A.R.S.M., F.G.S.</degrees>
<aff>The British Ceramic Research Association, Queen's Road, Penkhull, Stoke-on-Trent, Staffordshire</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>12</month>
<year>1956</year>
</pub-date>
<volume>31</volume>
<issue>235</issue>
<fpage>328</fpage>
<lpage>332</lpage>
<copyright-statement>Copyright &#x00A9; 1956, The Mineralogical Society</copyright-statement>
<copyright-year>1956</copyright-year>
<abstract>
<title>Summary</title>
<p>Sepiolite has been identified in the Keuper Marl at a Midlands locality by X-ray diffraction data, electron microscopy, differential thermal analysis, and chemical analysis. It has been calculated that a sample representing 30 ft. thickness of clay may contain as much as 39 % sepiolite. Apart from sepiolite, the Keuper Marl in the area examined consists mainly of mica, quartz, calcite, and ferric oxide.</p></abstract>
</article-meta>
</front>
</article>
