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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.1986.050.355.18</article-id>
<article-categories>
<subj-group subj-group-type="heading">
<subject>Mineralogy</subject>
</subj-group>
</article-categories>
<title-group>
<article-title>The Descloizite-Mottramite Series of Vanadates from the Otavi Mountain Land, South West Africa: An X-Ray Study</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>van der Westhuizen</surname>
<given-names>W. A.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>de Bruiyn</surname>
<given-names>H.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Tordiffe</surname>
<given-names>E. A. W.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Botha</surname>
<given-names>B. J. V.</given-names>
</name></contrib>
<aff>Department of Geology, University of the Orange Free State, PO Box 339, Bloemfontein, South Africa</aff></contrib-group>
<pub-date pub-type="ppub">
<month>3</month>
<year>1986</year>
</pub-date>
<volume>50</volume>
<issue>355</issue>
<fpage>137</fpage>
<lpage>140</lpage>
<history>
<date date-type="received">
<day>12</day>
<month>3</month>
<year>1984</year>
</date>
<date date-type="rev-recd">
<day>31</day>
<month>5</month>
<year>1985</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1986, The Mineralogical Society</copyright-statement>
<copyright-year>1986</copyright-year>
<abstract>
<title>Abstract</title>
<p>Descloizite, cuprian descloizite, and mottramite from most of the known prospects and mines in the Otavi Mountain Land were sampled and subsequently analysed chemically and by X-ray diffraction. Unit cell parameters were refined with the aid of a computer program. It was found that, contrary to previous opinion, chemical parameters of these vanadates can be deduced from their X-ray powder data according to the equations (correlation coefficients in parenthesis):</p>
<p>ZnO = 75.369<italic>c</italic>&#x2212;0.119<italic>b</italic>&#x2212;31.177<italic>a</italic>&#x2212;456.512(0.9634)</p>
<p>Zn<sup>2+</sup> = 369.568<italic>c</italic> + 236.583<italic>b</italic> &#x2212; 146.42<italic>a</italic> &#x2212; 3726.344 (0.9642)</p>
<p>CuO = &#x2212; 74.991<italic>c</italic> + 0.086<italic>b</italic> + 29.419<italic>a</italic> + 486.204 (0.9649)</p>
<p>Cu<sup>2+</sup> = &#x2212; 369.568<italic>c</italic> &#x2212; 236.583<italic>b</italic> + 146.420<italic>c</italic> + 3826.344 (0.9642).</p></abstract>
<kwd-group>
<title>Keywords</title>
<kwd>descloizite</kwd>
<kwd>mottramite</kwd>
<kwd>X-ray data</kwd>
<kwd>Otavi Mountain Land</kwd>
<kwd>South West Africa</kwd>
</kwd-group>
</article-meta>
</front>
</article>
