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<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.1934.023.146.03</article-id>
<title-group>
<article-title>Lusakite, a Cobalt-Bearing Silicate from Northern Rhodesia</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Skerl</surname>
<given-names>A. C.</given-names>
</name><degrees>A.R.S.M., B.Sc.</degrees>
<aff>Rhodesian Beit Railway Fellow at the Royal School of Mines, London</aff></contrib>
<contrib contrib-type="author">
<name>
<surname>Bannister</surname>
<given-names>F. A.</given-names>
</name><degrees>M.A.</degrees>
<aff>Assistant-Keeper in the Mineral Department of the British Museum of Natural History</aff></contrib>
<contrib contrib-type="author">
<name>
<surname>Groves</surname>
<given-names>A. W.</given-names>
</name><degrees>Ph.D., M.Sc., D.I.C., F.G.S.</degrees>
<aff>Geochemistry Department, Imperial College of Science and Technology, London</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>9</month>
<year>1934</year>
</pub-date>
<volume>23</volume>
<issue>146</issue>
<fpage>598</fpage>
<lpage>606</lpage>
<copyright-statement>Copyright &#x00A9; 1934, The Mineralogical Society</copyright-statement>
<copyright-year>1934</copyright-year>
<abstract>
<title>Summary</title>
<p>Lusakite is a cobalt-bearing variety of staurolite from Northern Rhodesia and has been named after the new capital of that colony. The orthorhombic crystals have unit-cell dimensions <italic>a</italic> 7&#x00B7;86, <italic>b</italic> 16&#x00B7;62, <italic>c</italic> 5&#x00B7;65 &#x00C5;. (<italic>a: b: c</italic> = 0&#x00B7;473: 1: 0&#x00B7;340), space-group <inline-formula><mml:math><mml:mrow><mml:msubsup><mml:mrow><mml:mi>V</mml:mi></mml:mrow><mml:mrow><mml:mi>h</mml:mi></mml:mrow><mml:mrow><mml:mn>17</mml:mn></mml:mrow></mml:msubsup></mml:mrow></mml:math></inline-formula>, and the unit cell contains 8[RO.Al<sub>2</sub>SiO<sub>5</sub>], where R = Fe,Co,Ni,Mg,Al,H. The empirical formula is H<sub>2</sub>O.4(Fe,Co,Ni,Mg)O.9(Al,Fe)<sub>2</sub>O<sub>3</sub>.8SiO<sub>2</sub>. Hardness 7 &#x00BD; specific gravity 3&#x00B7;767, <italic>n</italic> about 1&#x00B7;74. The following striking features justify the new name:
<list list-type="roman-lower list.lib">
<list-item><p>It is the only silicate mineral containing a significant amount of cobalt (CoO 8&#x00B7;48 %).</p></list-item>
<list-item><p>An intense cobalt-blue colour best seen in thin sections under the microscope.</p></list-item>
<list-item><p>Strong pleochroism from light cobalt-blue to deep violet-blue.</p></list-item>
<list-item><p>It has been formed by the metasomatic replacement of kyanite.</p></list-item></list></p></abstract>
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