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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.1990.054.377.12</article-id>
<article-categories>
<subj-group subj-group-type="heading">
<subject>Mineralogy and Petrology</subject>
</subj-group>
</article-categories>
<title-group>
<article-title>Corkite from Aggeneys, Bushmanland, South Africa</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>de Bruiyn</surname>
<given-names>H.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>van der Westhuizen</surname>
<given-names>W. A.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Beukes</surname>
<given-names>G. J.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Meyer</surname>
<given-names>T. Q.</given-names>
</name></contrib>
<aff>Department of Geology, University of the Orange Free State, PO Box 339, Bloemfontein 9300, South Africa</aff></contrib-group>
<pub-date pub-type="ppub">
<month>12</month>
<year>1990</year>
</pub-date>
<volume>54</volume>
<issue>377</issue>
<fpage>603</fpage>
<lpage>608</lpage>
<history>
<date date-type="received">
<day>8</day>
<month>1</month>
<year>1990</year>
</date>
<date date-type="rev-recd">
<day>1</day>
<month>5</month>
<year>1990</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1990, The Mineralogical Society</copyright-statement>
<copyright-year>1990</copyright-year>
<abstract>
<title>Abstract</title>
<p>Corkite associated with plumbojarosite and goethite occurs in gossan and iron-formation at Black Mountain and Broken Hill, Aggeneys. Electron microprobe analyses indicate that there are two groups of corkite present in the area; one with high Cu and low (PO<sub>4</sub>)<sup>3&#x2212;</sup> and the other with low Cu and high (PO and the other with low Cu and high (PO<sub>4</sub>)<sup>3&#x2212;</sup> contents. This can be explained in terms of the general formula contents. This can be explained in terms of the general formula <italic>AB</italic><sub>2</sub>(<italic>XO</italic><sub>4</sub>)<sub>2</sub>(OH)<sub>6</sub>, where the incorporation of divalent ions in the <italic>B</italic> site is accompanied by the exchange of trivalent anions by divalent ones to retain charge balance. Complete solid-solution is inferred between (SO<sub>4</sub>)<sup>2&#x2212;</sup>and (PO<sub>4</sub>)<sup>3&#x2212;</sup> end members, indicating that the jarosite and beudantite groups form part of the same solid-solution series. The distribution of Zn in corkite also reflects the regional distribution of zinc grades in the area, becoming more zinc-rich from west to east. New X-ray diffraction parameters are also presented which update existing data.</p></abstract>
<kwd-group>
<title>Keywords</title>
<kwd>corkite</kwd>
<kwd>EMP analyses</kwd>
<kwd>solid-solution series</kwd>
<kwd>X-ray diffraction data</kwd>
<kwd>Bushmanland</kwd>
<kwd>South Africa</kwd>
</kwd-group>
</article-meta>
</front>
</article>
