<?xml version="1.0"?>
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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.1989.053.371.03</article-id>
<article-categories>
<subj-group subj-group-type="heading">
<subject>Non-silicate Mineralogy</subject>
</subj-group>
</article-categories>
<title-group>
<article-title>Members of the Freibergite-Argentotennantite Series and Associated Minerals from Silvermines, County Tipperary, Ireland</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Zakrzewski</surname>
<given-names>Marek A.</given-names>
</name>
<aff>Institute of Earth Sciences, Free University, De Boelelaan 1085, 1081 HV Amsterdam, The Netherlands</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>6</month>
<year>1989</year>
</pub-date>
<volume>53</volume>
<issue>371</issue>
<fpage>293</fpage>
<lpage>298</lpage>
<history>
<date date-type="received">
<day>24</day>
<month>6</month>
<year>1988</year>
</date>
<date date-type="rev-recd">
<day>00</day>
<month>11</month>
<year>1988</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1989, The Mineralogical Society</copyright-statement>
<copyright-year>1989</copyright-year>
<abstract>
<title>Abstract</title>
<p>Ore microscope and electron microprobe investigations on Zn-Pb-Ag ores from B Zone in Silvermines, Ireland, have shown the presence of two As-Sb-Ag phases; a tetrahedrite-group mineral with composition Cu<sub>6.3</sub>Ag<sub>3.7</sub>Fe<sub>0.9</sub>Zn<sub>1.2</sub>As<sub>2.2</sub>Sb<sub>2.1</sub>S<sub>12.7</sub> and proustite-pyrargyrite (Ag<sub>3</sub>As<sub>0.5</sub>Sb<sub>0.5</sub>S<sub>3</sub>). It is postulated that both phases inherited their As and Sb from primary geocronite (Pb<sub>14.5</sub>As<sub>3.4</sub>Sb<sub>2.6</sub>S<sub>23</sub>) and that they are metastable. An enrichment in Ni in the ores is due to very fine to submicroscopic intergrowths of gersdorffite (Ni<sub>0.6</sub>Fe<sub>0.4</sub>AsS) with geocronite and with galena.</p></abstract>
<kwd-group>
<title>Keywords</title>
<kwd>freibergite</kwd>
<kwd>argentotennantite</kwd>
<kwd>tetrahedrite group</kwd>
<kwd>Silvermines</kwd>
<kwd>Ireland</kwd>
</kwd-group>
</article-meta>
</front>
</article>
