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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.1996.060.400.01</article-id>
<article-categories>
<subj-group subj-group-type="heading">
<subject>Mineralogy</subject>
</subj-group>
</article-categories>
<title-group>
<article-title>Cadmium Substitution in Miargyrite (AgSbS<sub>2</sub>) and Related Phases: An Experimental Reconnaissance</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Kelleher</surname>
<given-names>I.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Redfern</surname>
<given-names>S. A. T.</given-names>
</name></contrib>
<aff>Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge, UK</aff></contrib-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Pattrick</surname>
<given-names>R. A. D.</given-names>
</name>
<aff>Department of Earth Sciences, The University of Manchester, Manchester, M13 9PL, UK</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>6</month>
<year>1996</year>
</pub-date>
<volume>60</volume>
<issue>400</issue>
<fpage>393</fpage>
<lpage>401</lpage>
<history>
<date date-type="received">
<day>5</day>
<month>3</month>
<year>1993</year>
</date>
<date date-type="rev-recd">
<day>20</day>
<month>6</month>
<year>1995</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1996, The Mineralogical Society</copyright-statement>
<copyright-year>1996</copyright-year>
<abstract>
<title>Abstract</title>
<p>An experimental study of cadmium substitution into Ag<italic>X</italic>S<sub>2</sub> phases (X &#x003D; As, Bi, Sb) indicates significant amounts of cadmium can be incorporated in the structure by the mechanism 2Cd &#x21CC; Ag + <italic>X</italic>. The limit of substitution of Cd in the high-temperature polymorph of miargyrite, &#x03B2;-AgSbS<sub>2</sub> is 6.2 at.&#x0025;, whereas the low-temperature polymorph, &#x03B1;-AgSbS<sub>2</sub>, can accommodate at least 12 at.&#x0025; cadmium. Substitution of Cd into the cubic &#x03B2;-AgSbS<sub>2</sub> induces a small monoclinic distortion and the unit cell becomes pseudo-cubic. The &#x03B1; &#x21CC; &#x03B2; transition in Cd-substituted miargyrites is modified by the solute ions, with both a reduction of <italic>T</italic><sub>c</sub> and transition smearing evident. Similar effects are also recorded in Cd-substituted AgAsS<sub>2</sub> and AgBiS<sub>2</sub>.</p></abstract>
<kwd-group>
<title>Keywords</title>
<kwd>cadmium substitution</kwd>
<kwd>miargyrite</kwd>
<kwd>As</kwd>
<kwd>Bi</kwd>
<kwd>Sb</kwd>
</kwd-group>
</article-meta>
</front>
</article>
