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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.1958.031.242.08</article-id>
<title-group>
<article-title>Minium from Broken Hill, New South Wales</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Skinner</surname>
<given-names>Brian J.</given-names>
</name><degrees>B.Sc., M.A., Ph.D.</degrees></contrib>
<contrib contrib-type="author">
<name>
<surname>McBriab</surname>
<given-names>E. Maud.</given-names>
</name></contrib>
<aff>Geology Department, University of Adelaide, South Australia.</aff></contrib-group>
<pub-date pub-type="ppub">
<month>9</month>
<year>1958</year>
</pub-date>
<volume>31</volume>
<issue>242</issue>
<fpage>947</fpage>
<lpage>950</lpage>
<copyright-statement>Copyright &#x00A9; 1958, The Mineralogical Society</copyright-statement>
<copyright-year>1958</copyright-year>
<abstract>
<title>Summary</title>
<p>Minium occurs at Broken Hill, New South Wales, as pseudomorphs after cerussite, formed during fires in the mine. It is tetragonal with <italic>a</italic> = 8&#x00B7;824 &#x00C5;. and <italic>c</italic> = 6&#x00B7;564 &#x00C5;.; sp. gr. 8&#x00B7;2 + 0&#x00B7;2. The Broken Hill minium appears identical in physical properties with synthetic Pb<sub>3</sub>O<sub>4</sub> described by other workers.</p></abstract>
</article-meta>
</front>
</article>
