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<article article-type="research-article">
<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.1956.031.234.07</article-id>
<title-group>
<article-title>Some New Occurrences of Gonnardite</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Meixner</surname>
<given-names>H.</given-names>
</name> <degrees>Ph.D.</degrees>
<aff>Bergdirektion, H&#x00FC;ttenberg, Carinthia, Austria</aff></contrib>
<contrib contrib-type="author">
<name>
<surname>Hey</surname>
<given-names>M. H.</given-names>
</name> <degrees>M.A., D.Sc.</degrees></contrib>
<contrib contrib-type="author">
<name>
<surname>Moss</surname>
<given-names>A. A.</given-names>
</name> <degrees>B.Sc., Ph.D., F.S.A.</degrees></contrib>
<aff>Department of Mineralogy, British Museum</aff></contrib-group>
<pub-date pub-type="ppub">
<month>9</month>
<year>1956</year>
</pub-date>
<volume>31</volume>
<issue>234</issue>
<fpage>265</fpage>
<lpage>271</lpage>
<copyright-statement>Copyright &#x00A9; 1956, The Mineralogical Society</copyright-statement>
<copyright-year>1956</copyright-year>
<abstract>
<title>Summary</title>
<p>This zeolite, hitherto recorded only from Chaux de Bergonne, France, has been found as zoned spherules with thomsonite (var. faroelite), on specimens from Aci Castello and Aci Trezza, Sicily, and Capo di Bove, Rome, from Weilberg, Rhineland, and from Kl&#x00F6;ch, Styria. Three chemical analyses confirm previous results; optical data suggest some variation in composition within a spherule. There is a striking resemblance between X-ray fibre photographs of gonnardite and of thomsonite, and between X-ray powder photographs of gonnardire and of natrolite. The Kl&#x00F6;ch occurrence, where the gonnardite is accompanied by phillipsite, is described in detail.</p></abstract>
</article-meta>
</front>
</article>
