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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.1979.043.328.10</article-id>
<title-group>
<article-title>Wolfeite and Barbosalite from Thackaringa, Australia</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Plimer</surname>
<given-names>I. R.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Blucher</surname>
<given-names>I. D.</given-names>
</name></contrib>
<aff>University of New South Wales, P.O. Box 334, Broken Hill, NSW 2880, Australia</aff></contrib-group>
<pub-date pub-type="ppub">
<month>12</month>
<year>1979</year>
</pub-date>
<volume>43</volume>
<issue>328</issue>
<fpage>505</fpage>
<lpage>507</lpage>
<history>
<date date-type="received">
<day>8</day>
<month>2</month>
<year>1979</year>
</date>
<date date-type="rev-recd">
<day>1</day>
<month>6</month>
<year>1979</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1979, The Mineralogical Society</copyright-statement>
<copyright-year>1979</copyright-year>
<abstract>
<title>Summary</title>
<p>Wolfeite (Fe,Mn)<sub>2</sub>PO<sub>4</sub>(OH) and barbosalite Fe<sup>II</sup>Fe<sup>III</sup> <sub>2</sub>(PO<sub>4</sub>)<sub>2</sub>(OH)<sub>2</sub> are the principal phases in phosphate pods from the core of a zoned altered granitic pegmatite at Thackaringa. Chemical analyses of the wolfeite show it to be Fe-rich and extends the triploiditewolfeite isomorphous series (Frondel, 1949) from &#x03A3;Fe/Mn = 3&#x00B7;39 (this study) to greater than 100 (Clark and Couper, 1979).</p></abstract>
</article-meta>
</front>
</article>
