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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.1992.056.382.07</article-id>
<article-categories>
<subj-group>
<subject>Mineralogy and Petrology</subject>
</subj-group>
</article-categories>
<title-group>
<article-title>A New Occurrence of Vesigni&#x00E9;ite from the Gorob-Hope Copper Deposit, Namibia</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Schneider</surname>
<given-names>G. I. C.</given-names>
</name>
<aff>Geological Survey of Namibia P.O. Box 2168 Windhoek 9000, Namibia</aff></contrib>
<contrib contrib-type="author">
<name>
<surname>Lauenstein</surname>
<given-names>H. -J.</given-names>
</name>
<aff>Tsumeb Corporation P.O. Box 40 Tsumeb 9000, Namibia</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>3</month>
<year>1992</year>
</pub-date>
<volume>56</volume>
<issue>382</issue>
<fpage>67</fpage>
<lpage>69</lpage>
<history>
<date date-type="received">
<day>19</day>
<month>10</month>
<year>1989</year>
</date>
<date date-type="rev-recd">
<day>20</day>
<month>7</month>
<year>1991</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1992, The Mineralogical Society</copyright-statement>
<copyright-year>1992</copyright-year>
<abstract>
<title>Abstract</title>
<p>An iron-rich vesigni&#x00E9;ite, [Ba(Cu,Fe)<sub>3</sub>(VO<sub>4</sub>)<sub>2</sub>(OH)<sub>2</sub>] with Cu : Fe near 4 : 1, was identified in samples from the submarine-exhalative Gorob-Hope copper deposit, Namibia. The olive-colour mineral occurs as mammillary encrustations and vein fillings in the gossan zone of this deposit; it often has a brownish oxidation coating. The main X-ray lines are 3.21 &#x00C5; (100) [204, 113], 2.72 &#x00C5; (63) [313, 002] and 2.94 &#x00C5; (61) [020, 311]. The cell parameters are <italic>a</italic> = 10.236, <italic>b</italic> = 5.905, <italic>c</italic> = 14.253 &#x00C5; and &#x00DF; = 103.71&#x00B0;. The formation of vesigni&#x00E9;ite took place during the alteration of the ore under strongly alkaline and slightly reducing to oxidizing conditions. While copper and barium were derived from the submarine exhalative mineralisation, vanadium was leached from the countryrock, a micea schist.</p></abstract>
<kwd-group>
<title>Keywords</title>
<kwd>vesigni&#x00E9;ite</kwd>
<kwd>vanadate</kwd>
<kwd>Gorob-Hope deposit</kwd>
<kwd>Namibia</kwd>
</kwd-group>
</article-meta>
</front>
</article>
