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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.1972.038.299.03</article-id>
<title-group>
<article-title>The New Mineral Insizwaite (PtBi<sub>2</sub>) and New Data on Niggliite (PtSn)</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Cabri</surname>
<given-names>L. J.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Harris</surname>
<given-names>D. C.</given-names>
</name></contrib>
<aff>Mineral Sciences Division, Department of Energy, Mines and Resources, Mines Branch, 555 Booth Street, Ottawa, Canada. K1A 0G1</aff></contrib-group>
<pub-date pub-type="ppub">
<month>9</month>
<year>1972</year>
</pub-date>
<volume>38</volume>
<issue>299</issue>
<fpage>794</fpage>
<lpage>800</lpage>
<history>
<date date-type="received">
<day>7</day>
<month>2</month>
<year>1972</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1972, The Mineralogical Society</copyright-statement>
<copyright-year>1972</copyright-year>
<abstract>
<title>Summary</title>
<p>Insizwaite from Waterfall Gorge, Insizwa, is a new mineral with the composition Pt<sub>1&#x00B7;00</sub>Bi<sub>1&#x00B7;35</sub>Sb<sub>0&#x00B7;57</sub>. The name is for the locality and is to be applied to the end member PtBi<sub>2</sub>. The analysed material is an antimonian variety. The mineral is cubic, the unit-cell for the antimonian variety has <italic>a</italic> 6&#x00B7;625 (2) &#x00C5;, probable space group <italic>Pa</italic>3, calc. D 12&#x00B7;8 g/cm<sup>3</sup>. The strongest lines on the X-ray diffraction powder pattern are: 2&#x00B7;96 (8) 210; 2&#x00B7;70 (8) 211; 2&#x00B7;34 (5) 220; 1&#x00B7;99 (10 311; 1&#x00B7;774 (7) 321; 1&#x00B7;433 (5) 421; 1&#x00B7;277 (6) 511, 333; 1&#x00B7;171 (6) 440; and 0&#x00B7;862 (7) 731. Under reflected light the mineral is white (in air and in oil) and is isotropic. Reflectance measurements at 470, 546, 589, and 650 nm gave 61&#x00B7;1, 60&#x00B7;0, 60&#x00B7;6, and 61&#x00B7;7 %. Micro-indentation hardness values range from 488 to 540 (av. 519) kg/mm<sup>2</sup> with a 25 g load.</p>
<p>New data are presented for niggliite from the type locality and for synthetic PtSn.</p></abstract>
</article-meta>
</front>
</article>
