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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.1984.048.349.10</article-id>
<title-group>
<article-title>The Crystal Structure of Caratiite</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Effenberger</surname>
<given-names>Herta</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Zemann</surname>
<given-names>Josef</given-names>
</name></contrib>
<aff>Institut f&#x00FC;r Mineralogie und Kristallographie, Universit&#x00E4;t Wien, Dr. Karl Lueger-Ring 1, A-1010 Wien, Austria</aff></contrib-group>
<pub-date pub-type="ppub">
<month>12</month>
<year>1984</year>
</pub-date>
<volume>48</volume>
<issue>349</issue>
<fpage>541</fpage>
<lpage>546</lpage>
<history>
<date date-type="received">
<day>20</day>
<month>4</month>
<year>1984</year>
</date>
<date date-type="rev-recd">
<day>29</day>
<month>6</month>
<year>1984</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1984, The Mineralogical Society</copyright-statement>
<copyright-year>1984</copyright-year>
<abstract>
<title>Abstract</title>
<p>The crystal structure of caratiite, K<sub>4</sub>Cu<sub>4</sub>O<sub>2</sub> (SO<sub>4</sub>)<sub>4</sub><italic>Me</italic>Cl (<italic>a</italic> 13.60(2), <italic>c</italic> 4.98(1) &#x00C5;, Z = 2) was solved in space group <italic>I</italic>4 from single crystal data, and refined to R = 0.035 for 654F<sub>o</sub> &#x003E; 6<italic>&#x03C3;</italic>(F<sub>o</sub>). The atomic arrangement is characterized by Cu<sub>2</sub>O(SO<sub>4</sub>)<sub>2</sub> chains parallel to [001], with Cu in (4 + 1) co-ordination and O surrounded tetrahedrally by four Cu atoms. These chains are interconnected by K atoms to a framework, the channels of which house the <italic>Me</italic> and Cl atoms. The nature of the <italic>Me</italic> atoms is not completely clear; most probably the position is half occupied by Cu, fully occupied by Na, or occupied by a mixture of the two.</p></abstract>
</article-meta>
</front>
</article>
