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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.1970.037.290.02</article-id>
<title-group>
<article-title>Hodrushite&#x2014;A New Sulphosalt</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Kod&#x011B;ra</surname>
<given-names>M.</given-names>
</name>
<aff>Department of Mineralogy and Crystallography, Comenius University, Bratislava, Czechoslovakia</aff></contrib>
<contrib contrib-type="author">
<name>
<surname>Kup&#x010D;ik</surname>
<given-names>V.</given-names>
</name>
<aff>Institut f&#x00FC;r Mineralogie und Kristallographie, Universit&#x00E4;t G&#x00F6;ttingen, Germany</aff></contrib>
<contrib contrib-type="author">
<name>
<surname>Makovick&#x00FD;</surname>
<given-names>E.</given-names>
</name>
<aff>McGill University, Montreal, Canada</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>6</month>
<year>1970</year>
</pub-date>
<volume>37</volume>
<issue>290</issue>
<fpage>641</fpage>
<lpage>648</lpage>
<history>
<date date-type="received">
<day>20</day>
<month>6</month>
<year>1967</year>
</date>
<date date-type="rev-recd">
<day>7</day>
<month>7</month>
<year>1969</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1970, The Mineralogical Society</copyright-statement>
<copyright-year>1970</copyright-year>
<abstract>
<title>Summary</title>
<p>Hodrushite, a new sulphosalt of copper and bismuth, was found in the Rosalia ore vein at Bansk&#x00E1; Hodru&#x00E1; near Bansk&#x00E1; &#x0160;tiavnica, Czechoslovakia. It has chemical composition Cu<sub>8&#x00B7;12</sub>Bi<sub>11&#x00B7;54</sub>Fe<sub>0&#x00B7;29</sub>S<sub>22</sub>(as determined by electron-microprobe method) close to Cu<sub>8</sub>Bi<sub>12</sub>S<sub>22</sub>. Symmetry is monoclinic, space group <italic>A</italic>2/<italic>m</italic>, lattice constants <italic>a</italic> 27&#x00B7;21, <italic>b</italic> 3&#x00B7;93, <italic>c</italic> 17&#x00B7;58 &#x00C5;, <italic>&#x03B2;</italic> 92&#x00B0; 9&#x2032;, measured density 6&#x00B7;35, calculated density 6&#x00B7;45 g/cm<sub>3</sub>. Microhardness 200 kg/mm<sub>2</sub>, anisotropic, weak bireflectance, creamy with pinkish tint, maximum reflectivity about 6000 &#x00C5;. Crystals needle-shaped and striated along [010], colour steel-grey, quickly tarnishing to bronze. Associated with quartz, hematite, and chalcopyrite. Closely related to cuprobismutite.</p></abstract>
</article-meta>
</front>
</article>
