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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.1904.014.63.06</article-id>
<title-group>
<article-title>On Teallite, a New Sulphostannite of Lead from Bolivia; and its Relations to Franckeite and Cylindrite</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Prior</surname>
<given-names>G. T.</given-names>
</name><degrees>M.A., F.G.S.</degrees>
<aff>Assistant in the Mineral Department of the British Museum.</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>10</month>
<year>1904</year>
</pub-date>
<volume>14</volume>
<issue>63</issue>
<fpage>21</fpage>
<lpage>27</lpage>
<copyright-statement>Copyright &#x00A9; 1904, The Mineralogical Society</copyright-statement>
<copyright-year>1904</copyright-year>
<abstract>
<title>Summary</title>
<p><italic>Characters of Teallite</italic>:&#x2014;</p>
<p>Grey-black colour, metallic lustre, soils paper like graphite, occurs in flexible folia with nearly square outline, perfect basal cleavage, hardness, 1&#x2013;2, does not scratch gypsum, density, 6&#x00B7;36. Orthorhombic, <italic>a</italic>:<italic>b</italic>:<italic>r</italic> = 0&#x00B7;93 : 1 : 1&#x00B7;31. Chemical formula, PbSnS<sub>2</sub>.</p>
<p><italic>Probable chemical formula of franckeite</italic>:&#x2014; Pb<sub>5</sub>FeSn<sub>3</sub>Sb<sub>2</sub>S<sub>14</sub> = 3PbSnS<sub>2</sub> + Pb<sub>2</sub>FeSb<sub>2</sub>S<sub>8</sub>.</p>
<p><italic>Probable chemical formula of cylindrite</italic>:&#x2014; Pb<sub>3</sub>FeSn<sub>4</sub>Sb<sub>2</sub>S<sub>14</sub> = 3PbSnS<sub>2</sub> + SnFeSb<sub>2</sub>S<sub>8</sub>.</p></abstract>
</article-meta>
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</article>
