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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.1990.054.377.14</article-id>
<article-categories>
<subj-group subj-group-type="heading">
<subject>Crystal Structures</subject>
</subj-group>
</article-categories>
<title-group>
<article-title>The Crystal Structure of Kamchatkite, a New Naturally Occurring Oxychloride Sulphate of Potassium and Copper</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Varaksina</surname>
<given-names>T. 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>Department of Crystallography, Leningrad State University, USSR,</aff></contrib-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Vergasova</surname>
<given-names>L. P.</given-names>
</name>
<aff>Institute of Volcanology, Academy of Sciences of the USSR, Petropavlovsk-Kamchatsky</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>12</month>
<year>1990</year>
</pub-date>
<volume>54</volume>
<issue>377</issue>
<fpage>613</fpage>
<lpage>616</lpage>
<history>
<date date-type="received">
<day>6</day>
<month>10</month>
<year>1989</year>
</date>
<date date-type="rev-recd">
<day>7</day>
<month>3</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>The crystal structure of the new mineral kamchatkite, <italic>a</italic>= 9.741(5), <italic>b</italic>= 12.858(6), <italic>c</italic>=7.001(3)&#x00C5;, space group <italic>Pna</italic>2<sub>1</sub>, Z = 4, has been determined through direct methods using 1430 intensities and refined to a final discrepancy index <italic>R</italic> = 0.055. It contains (SO<sub>4</sub>) tetrahedra and Cu octahedra interconnected by oxygen atoms to form an electrostatically neutral three-dimensional arrangement of formula Cu<sub>3</sub>O[SO<sub>4</sub>]<sub>2</sub> which contains channels parallel to [001]. The channels are not empty but house KCl molecules.</p></abstract>
<kwd-group>
<title>Keywords</title>
<kwd>kamchatkite</kwd>
<kwd>crystal structure</kwd>
<kwd>Kamchatka</kwd>
<kwd>USSR</kwd>
</kwd-group>
</article-meta>
</front>
</article>
