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<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.1975.040.311.03</article-id>
<title-group>
<article-title>Argentian Mercurian Tetrahedrite, a New Variety, from the Chiprovtsi Ore Deposit, Western Stara-Planina Mountains, Bulgaria</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Atanasov</surname>
<given-names>Vassil AT.</given-names>
</name>
<aff>Higher Institute of Mining and Geology, Sofia 56, Bulgaria</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>9</month>
<year>1975</year>
</pub-date>
<volume>40</volume>
<issue>311</issue>
<fpage>233</fpage>
<lpage>237</lpage>
<history>
<date date-type="received">
<day>15</day>
<month>7</month>
<year>1974</year>
</date>
<date date-type="rev-recd">
<day>13</day>
<month>9</month>
<year>1974</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1975, The Mineralogical Society</copyright-statement>
<copyright-year>1975</copyright-year>
<abstract>
<title>Summary</title>
<p>An electron-probe microanalysis of tetrahedrite occurring together with the latest-deposited pyrite-cinnabar association in the Chiprovtsi lead-silver deposit yielded more than 16 wt. % Ag and more than 18 wt. % Hg. X-ray powder examination established an extremely large unit-cell edge, <italic>a</italic> 10&#x00B7;64&#x00B1;0&#x00B7;01 &#x00C5;. Vickers microhardness 223 to 237 kg/mm<sup>2</sup>. The chemical formula derived on the basis of the analyses made is quite near to Cu<sub>6</sub><sup>+</sup>(Cu<sup>+</sup>, Ag<sup>+</sup>)<sub>4</sub>(Hg,Zn)<sub>2</sub>(Sb,As)<sub>4</sub>S<sub>113</sub>. There is not any antiparallelism between Ag and Hg in tetrahedrite. The name proposed for all stages of simultancous isomorphic replacement along the Cu<sup>+</sup>-Ag<sup>+</sup> and Cu<sup>2+</sup>-Hg<sup>2+</sup>(Zn<sup>2+</sup>,Fe<sup>2+</sup>) directions is argentian mercurian tetrahedrite. The upper limits of the Ag and Hg content are expected to be Cu<sub>6</sub>Ag<sub>4</sub>Hg<sub>2</sub>(Sb,As)<sub>4</sub>S<sub>13</sub>. It is the six copper atoms (<inline-formula><mml:math><mml:mrow><mml:msubsup><mml:mrow><mml:mi>Cu</mml:mi></mml:mrow><mml:mrow><mml:mn>4</mml:mn></mml:mrow><mml:mrow><mml:mo>&#x002B;</mml:mo></mml:mrow></mml:msubsup><mml:mo>&#x00B7;</mml:mo><mml:msubsup><mml:mrow><mml:mi>Cu</mml:mi></mml:mrow><mml:mrow><mml:mn>2</mml:mn></mml:mrow><mml:mrow><mml:mn>2</mml:mn><mml:mo>&#x002B;</mml:mo></mml:mrow></mml:msubsup></mml:mrow></mml:math></inline-formula>), sited in the Laves' polyhedra, that are replaced by Ag<sup>+</sup> and Hg<sup>2+</sup> respectively.</p></abstract>
</article-meta>
</front>
</article>
