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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.1997.061.408.05</article-id>
<title-group>
<article-title>Crystal Structure Refinement of Miargyrite, AgSbS<sub>2</sub></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Smith</surname>
<given-names>Joseph V.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Pluth</surname>
<given-names>Joseph J.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Han</surname>
<given-names>Shao-xu</given-names>
</name></contrib>
<aff>Department of Geophysical Sciences &#x0026; Center for Advanced Radiation Sources, University of Chicago, Chicago, Illinois 60637, USA</aff></contrib-group>
<pub-date pub-type="ppub">
<month>10</month>
<year>1997</year>
</pub-date>
<volume>61</volume>
<issue>408</issue>
<fpage>671</fpage>
<lpage>675</lpage>
<history>
<date date-type="received">
<day>24</day>
<month>9</month>
<year>1996</year>
</date>
<date date-type="rev-recd">
<day>22</day>
<month>1</month>
<year>1997</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1997, The Mineralogical Society</copyright-statement>
<copyright-year>1997</copyright-year>
<abstract>
<title>Abstract</title>
<p>Miargyrite is the low-temperature monoclinic derivative of a high temperature cubic galena/halite structure. The essential features of its crystal structure (Knowles, 1959) were confirmed, but the details of the bonding changed [new space group <italic>C</italic>121; <italic>a</italic> 12.824(1), <italic>b</italic> 4.4060(3), <italic>c</italic> 13.193(1) &#x00C5;, &#x03B2; 98.567(6)&#x00B0;]. The octahedral connectivity of galena/halite is severely distorted: Ag(1), 2S each at 2.53, 2.66 &#x0026; 3.39 &#x00C5;; Ag(2), 2 each at 2.54, 2.62 and 3.44; Ag(3), 2.38, 2.40, 3.05, 3.05, 3.53, 3.58; Sb(1), 2.45, 2.50, 2.51, 3.22 3.28, 3.41; Sb(2), 2.45, 2.50, 2.51, 3.22, 3.28, 3.41. The short distances define the following coordinations: very distorted tetrahedral Ag(1) and (2); near-linear Ag(3) at 178.9(2)&#x00B0; trigonal-pyramidal Sb(1) and (2) at 92.0, 93.6 and 96.8&#x00B0;. The ten shortest S-S distances range from 3.61 to 3.77 &#x00C5;.</p></abstract>
<kwd-group>
<title>Keywords</title>
<kwd>miargyrite</kwd>
<kwd>crystal stricture</kwd>
<kwd>AgSbS<sub>2</sub></kwd>
</kwd-group>
</article-meta>
</front>
</article>
