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<article article-type="research-article">
<front>
<journal-meta>
<journal-id journal-id-type="archive">gsminmag</journal-id>
<journal-title>Clay Minerals</journal-title>
<abbrev-journal-title abbrev-type="full">Clay Minerals</abbrev-journal-title>
<issn pub-type="ppub">0009-8558</issn>
<publisher>
<publisher-name>Mineralogical Society</publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.1180/minmag.1953.030.222.06</article-id>
<title-group>
<article-title>On the Occurrence of Nacrite at Shap, Westmorland</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Firman</surname>
<given-names>R. J.</given-names>
</name><degrees>B.Sc., F.G.S.</degrees>
<aff>Department of Geology, Durham Colleges in the University of Durham.</aff></contrib></contrib-group>
<author-notes>
<fn fn-type="com" id="FN1"><label>1</label><p>Communicated by the General Secretary; taken as read June 11, 1953.</p></fn></author-notes>
<pub-date pub-type="ppub">
<month>9</month>
<year>1953</year>
</pub-date>
<volume>30</volume>
<issue>222</issue>
<fpage>199</fpage>
<lpage>200</lpage>
<copyright-statement>Copyright &#x00A9; 1953, The Mineralogical Society</copyright-statement>
<copyright-year>1953</copyright-year>
</article-meta>
</front>
</article>
