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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.1970.037.290.08</article-id>
<title-group>
<article-title>Russellite: A Second Occurrence</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Hodge</surname>
<given-names>L. C.</given-names>
</name>
<aff>Government Chemical Laboratories, Perth, Western Australia</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>6</month>
<year>1970</year>
</pub-date>
<volume>37</volume>
<issue>290</issue>
<fpage>705</fpage>
<lpage>707</lpage>
<history>
<date date-type="received">
<day>5</day>
<month>8</month>
<year>1969</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1970, The Mineralogical Society</copyright-statement>
<copyright-year>1970</copyright-year>
<abstract>
<title>Summary</title>
<p>Russellite Bi<sub>2</sub>O<sub>3</sub>. WO<sub>3</sub> occurs in a small pegmatite near Poona, Western Australia. The fine-grained yellow to pale green material is an inseparable mixture of russellite, bismite, koechlinite, and bismutite. X-ray powder diffraction, physical, and chemical data agree in general with the original description of the mineral from Cornwall, England. The original analyses made on micro quantities are now supplemented by analyses on macro quantities.</p></abstract>
</article-meta>
</front>
</article>
