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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.1991.055.381.14</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 Fedotovite, K<sub>2</sub>Cu<sub>3</sub>O(SO<sub>4</sub>)<sub>3</sub></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>Filatov</surname>
<given-names>S. K.</given-names>
</name></contrib>
<aff>Department of Crystallography, Leningrad State University, Univers. Emb. 7/9, Leningrad 199164, USSR</aff></contrib-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Fundamensky</surname>
<given-names>V. S.</given-names>
</name>
<aff>INPO &#x2018;Burevestnik&#x2019;, Leningrad</aff></contrib>
<contrib contrib-type="author">
<name>
<surname>Vergasova</surname>
<given-names>L. P.</given-names>
</name>
<aff>Institute of Volcanology, the Academy of Sciences of the USSR, Petropavlovsk-Kamchatsky, USSR</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>12</month>
<year>1991</year>
</pub-date>
<volume>55</volume>
<issue>381</issue>
<fpage>613</fpage>
<lpage>616</lpage>
<history>
<date date-type="received">
<day>29</day>
<month>11</month>
<year>1989</year>
</date>
<date date-type="rev-recd">
<day>29</day>
<month>11</month>
<year>1990</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1991, The Mineralogical Society</copyright-statement>
<copyright-year>1991</copyright-year>
<abstract>
<title>Abstract</title>
<p>The crystal structure of fedotovite, K<sub>2</sub>Cu<sub>3</sub>O(SO<sub>4</sub>)<sub>3</sub> has been determined, space group <italic>C</italic>2/<italic>c</italic>, <italic>a</italic> 19.037(6), <italic>b</italic> 9.479(2), <italic>c</italic> 14.231(5) &#x00C5;, &#x03B2; 111.04(3)&#x00B0;, Z = 8, <italic>D</italic><sub>x</sub> = 3.09 g/cm<sup>3</sup>. The main units of the fedotovite structure are formed around two additional oxygen atoms and consist of edge-sharing [OCu<sub>4</sub>] tetrahedra and four [SO<sub>4</sub>] tetrahedra attached to them. The units are further connected by two [SO<sub>4</sub>] tetrahedra, building distinct layers parallel to the <italic>yz</italic> plane. These layers are interconnected by potassium atoms. In the fedotovite structure, the three kinds of copper atoms are fivefold (4 + 1) coordinated to oxygen atoms with a strong Jahn-Teller effect. The coordination polyhedra of Cu1 and Cu2 atoms are distorted and flattened orthorhombic pyramids with Cu-O distances varying from 1.912 to 2.333 &#x00C5;, the sixth neighbour of the both atoms is the copper atom lying at 2.975 and 2.981 &#x00C5; for Cu2 and Cu1 respectively. The coordination environment of the Cu3 atom is a distorted elongated orthorhombic pyramid with four Cu-O distances from 1.943 to 1.961 &#x00C5;, a fifth at 2.558 &#x00C5;, and further sixth and seventh neighbours (oxygen and copper atoms) at 2.809 and 2.806 &#x00C5;, respectively.</p></abstract>
<kwd-group>
<title>Keywords</title>
<kwd>fedotovite</kwd>
<kwd>crystal structure</kwd>
</kwd-group>
</article-meta>
</front>
</article>
