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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.1997.061.404.08</article-id>
<article-categories>
<subj-group>
<subject>Mineralogy</subject>
</subj-group>
</article-categories>
<title-group>
<article-title>The Crystal Chemistry of the Solid Solution Series between Chalcostibite (CuSbS<sub>2</sub>) and Emplectite (CuBiS<sub>2</sub>)</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Razmara</surname>
<given-names>M. F.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Henderson</surname>
<given-names>C. M. B.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Pattrick</surname>
<given-names>R. A. D.</given-names>
</name></contrib>
<aff>Department of Earth Sciences, University of Manchester, Manchester, M13 9PL, UK</aff></contrib-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Bell</surname>
<given-names>A. M. T.</given-names>
</name>
<xref ref-type="author-notes" rid="FN1">*</xref></contrib>
<contrib contrib-type="author">
<name>
<surname>Charnock</surname>
<given-names>J. M.</given-names>
</name></contrib>
<aff>Daresbury Laboratory, Warrington, WA4 4AD, UK</aff></contrib-group>
<author-notes>
<fn fn-type="current-aff" id="FN1"><label>*</label><p>Current address: Department of Chemistry, Lensfield Road, Cambridge CB2 1EP</p></fn></author-notes>
<pub-date pub-type="ppub">
<month>2</month>
<year>1997</year>
</pub-date>
<volume>61</volume>
<issue>404</issue>
<fpage>79</fpage>
<lpage>88</lpage>
<history>
<date date-type="received">
<day>26</day>
<month>4</month>
<year>1996</year>
</date>
<date date-type="rev-recd">
<day>31</day>
<month>7</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>Sulphosalts in the system CuSbS<sub>2</sub>-CuBiS<sub>2</sub> (chalcostibite-emplectite) form a complete solid solution series. Seven compositions with the general formula Cu(Sb<sub><italic>x</italic></sub>Bi<sub>l&#x2212;<italic>x</italic></sub>)S<sub>2</sub> have been synthesized using dry methods at 310&#x00B0;C. All members of the series are orthorhombic (space group <italic>Pnma</italic>) and show smoothly increasing <italic>a</italic> and <italic>b</italic> cell parameters with substitution of Bi for Sb; the <italic>c</italic> cell parameter increases up to 50% CuBiS<sub>2</sub> substitution and then becomes constant. DSC experiments on CuBiS<sub>2</sub> show an endothermic heat effect (2.45 kJ/mol.) at 472&#x00B0;C due to the breakdown reaction to Cu<sub>3</sub>BiS<sub>3</sub> (wittichenite) plus Bi<sub>2</sub>S<sub>3</sub> (bismuthinite). With the addition of 10% CuSbS<sub>2</sub> to CuBiS<sub>2</sub>, the decomposition temperature increases and the endothermic peak is broadened but the energy remains essentially the same (2.53 kJ/mol.). No evidence of this decomposition was observed when the amount of the CuSbS<sub>2</sub> component was &#x003E;30%. The local structure and co-ordination of Cu in the samples were studied by EXAFS analysis of the Cu-<italic>K</italic> edge but no significant variation occurs in the local Cu environment. The Debye-Waller factor for the first shell of S atoms surrounding Cu in end member CuSbS<sup>2</sup> tends to be slightly smaller than for the intermediate solid solutions, suggesting that the tetrahedral Cu environments in the intermediate composition samples is somewhat more disordered than in the end-member. The low expansion characteristics along <italic>c</italic> appear to be controlled by the linkages between the (CuS<sub>3</sub> + BiS<sub>2</sub>) sheets perpendicular to <italic>c</italic> being relatively inflexible.</p></abstract>
<kwd-group>
<title>Keywords</title>
<kwd>chalcostibite</kwd>
<kwd>emplectite</kwd>
<kwd>crystal chemistry</kwd>
<kwd>sulphosalts</kwd>
</kwd-group>
</article-meta>
</front>
</article>
