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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.1978.042.321.13</article-id>
<title-group>
<article-title>Linnaeite Series Minerals from the Kalgoorlie District, Western Australia</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Ostwald</surname>
<given-names>J.</given-names>
</name>
<aff>The Broken Hill Proprietary Company Limited, Central Research Laboratories, Shortland, N.S.W. 2307, Australia</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>3</month>
<year>1978</year>
</pub-date>
<volume>42</volume>
<issue>321</issue>
<fpage>93</fpage>
<lpage>98</lpage>
<history>
<date date-type="received">
<day>10</day>
<month>2</month>
<year>1977</year>
</date>
<date date-type="rev-recd">
<day>12</day>
<month>9</month>
<year>1977</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1978, The Mineralogical Society</copyright-statement>
<copyright-year>1978</copyright-year>
<abstract>
<title>Summary</title>
<p>Five members of the linnaeite series of sulphides linnaeite Co<sub>3</sub>S<sub>4</sub>, siegenite (Co, Ni)<sub>3</sub>S<sub>4</sub>, carrollite Co<sub>2</sub>CuS<sub>4</sub>, violarite Ni<sub>2</sub>FeS<sub>4</sub>, and polydymite Ni<sub>3</sub>S<sub>4</sub> occur in nickel-sulphide-mineralized rocks in areas adjacent to the Kambalda and Scotia deposits of the Kalgoorlie district, Western Australia. Linnaeite, siegenite, carrollite, and polydymite occur in trace amounts as disseminated grains and veinlets. Violarite is also found as disseminations but its major occurrence is in the supergene enriched zones of the ore deposits. Aspects of their mineralogy, including mode of occurrence, general mineragraphy, reflectance at 546 nm, 589 nm and 644 nm, microhardness, and electron probe microanalyses are described.</p></abstract>
</article-meta>
</front>
</article>
