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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.1983.047.345.05</article-id>
<title-group>
<article-title>Silver Substitution into Synthetic Zinc, Cadmium, and Iron Tetrahedrites</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Pattrick</surname>
<given-names>R. A. D.</given-names>
</name>
<aff>Department of Geology, The University, Manchester M13 9PL</aff></contrib>
<contrib contrib-type="author">
<name>
<surname>Hall</surname>
<given-names>A. J.</given-names>
</name>
<aff>Department of Applied Geology, University of Strathclyde, Glasgow</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>12</month>
<year>1983</year>
</pub-date>
<volume>47</volume>
<issue>345</issue>
<fpage>441</fpage>
<lpage>451</lpage>
<history>
<date date-type="rev-recd">
<day>27</day>
<month>6</month>
<year>1983</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1983, The Mineralogical Society</copyright-statement>
<copyright-year>1983</copyright-year>
<abstract>
<title>Abstract</title>
<p>The limits and effect on cell size of silver substitution into synthetic tetrahedrite, Cu<sub>10</sub>(Zn,Fe,Cd<sub>2</sub>) Sb<sub>4</sub>S<sub>13</sub>, are investigated for comparison with natural tetrahedrite. The limit of Ag substitution into natural zincian tetrahedrite is &#x223C; 4 atoms per half unit cell and into iron tetrahedrite &#x223C; 6.5 atoms (with rare exceptions). The cell size of natural tetrahedrite increases with increasing Ag content up to 4 atoms but decreases with further Ag substitution. The highest Ag substitution achieved in synthetic tetrahedrites was 4.7 atoms in Zn<sub>2</sub>-tetrahedrite, 7.02 atoms in Cd<sub>2</sub>-tetrahedrite and 6.80 atoms in Fe<sub>2</sub>-tetrahedrite. The cell size of synthetic tetrahedrites shows a continuous increase with increasing Ag content, the largest cell size of <italic>a</italic> = 10.927 &#x00C5; being in the Cd<sub>2</sub>-tetrahedrite with 7.02 atoms Ag. The iron content of tetrahedrite systematically increased from 1.1 to 2.0 atoms per half unit cell tetrahedrite with increase from 0 to &#x223C; 4 atoms Ag. The different limit of Ag substitution between Zn<sub>2</sub> and Cd<sub>2</sub> tetrahedrite can be explained by size constraints on the expanding structure. An explanation is given for a limit of 7 atoms Ag substitution in tetrahedrite using a combined electron band/molecular orbital approach.</p></abstract>
</article-meta>
</front>
</article>
