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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.1997.061.406.09</article-id>
<article-categories>
<subj-group subj-group-type="heading">
<subject>Crystal Structure</subject>
</subj-group>
</article-categories>
<title-group>
<article-title>The Crystal Structure of Averievite, Cu<sub>5</sub>O<sub>2</sub>(VO<sub>4</sub>)<sub>2</sub>&#x00B7;n<italic>MX</italic>: Comparison with Related Compounds</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Starova</surname>
<given-names>G. L.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Krivovichev</surname>
<given-names>S. V.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Fundamensky</surname>
<given-names>V. S.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Filatov</surname>
<given-names>S. K.</given-names>
</name></contrib>
<aff>Departament of Crystallography, Saint-Petersburg State University, University Emb. 7/9, St.Petersburg, 199034, Russia</aff></contrib-group>
<pub-date pub-type="ppub">
<month>6</month>
<year>1997</year>
</pub-date>
<volume>61</volume>
<issue>406</issue>
<fpage>441</fpage>
<lpage>446</lpage>
<history>
<date date-type="received">
<day>8</day>
<month>2</month>
<year>1996</year>
</date>
<date date-type="rev-recd">
<day>3</day>
<month>9</month>
<year>1996</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1997, The Mineralogical Society</copyright-statement>
<copyright-year>1997</copyright-year>
<abstract>
<title>Abstract</title>
<p>The crystal structure of averievite, Cu<sub>5</sub>O<sub>2</sub>(VO<sub>4</sub>)<sub>2</sub>&#x00B7;n<italic>MX</italic> has been determined. Trigonal system, space group <italic>P</italic>3, <italic>a</italic> = 6.375(1), <italic>c</italic> = 8.399(1) &#x00C5;, V = 295.6(1) &#x00C5;<sup>3</sup>, Z = 1, D<sub>x</sub> = 4.01(1) g/cm<sup>3</sup>. The atomic arrangement is characterized by infinite nets parallel to (001) composed of [OCu<sub>4</sub>]<sup>6+</sup> tetrahedra linked via corners in hexagonal rings. The bases of neigbouring tetrahedra are in one plane and their non-shared corners are turned to the opposite sides. The [VO<sub>4</sub>]<sup>3&#x2212;</sup> tetrahedra are attached to the bases of [OCu<sub>4</sub>] tetrahedra. There are large (R &#x003E;3.2 &#x00C5;) channels in the structure where large molecular particles can enter. The comparison of the averievite structure with related compounds (in particular, copper oxovanadates) is given from the point of view of [O<italic>T</italic><sub>4</sub>] polyion crystal chemistry.</p></abstract>
<kwd-group>
<title>Keywords</title>
<kwd>averievite</kwd>
<kwd>crystal structure</kwd>
</kwd-group>
</article-meta>
</front>
</article>
