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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.1968.036.281.06</article-id>
<title-group>
<article-title>On the Composition of Natural Delafossite</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Hey</surname>
<given-names>M. H.</given-names>
</name>
<aff>Department of Mineralogy, British Museum (Natural History), London, S.W. 7</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>3</month>
<year>1968</year>
</pub-date>
<volume>36</volume>
<issue>281</issue>
<fpage>651</fpage>
<lpage>653</lpage>
<history>
<date date-type="received">
<day>15</day>
<month>8</month>
<year>1967</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1968, The Mineralogical Society</copyright-statement>
<copyright-year>1968</copyright-year>
<abstract>
<title>Summary</title>
<p>Two new microanalyses of delafossite from Nizhnii Tagil (the type locality) and Kimberly, Nevada, confirm the accepted formula CuFeO<sub>2</sub>.</p></abstract>
</article-meta>
</front>
</article>
