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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.1975.040.309.09</article-id>
<title-group>
<article-title>A Garnierite with a High Nickel Content from Western Australia</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Nickel</surname>
<given-names>E. H.</given-names>
</name>
<aff>Division of Mineralogy, CSIRO, Wembley, W.A., Australia, 6014</aff></contrib>
<contrib contrib-type="author">
<name>
<surname>Bridge</surname>
<given-names>P. J.</given-names>
</name>
<aff>Government Chemical Laboratories, Perth, W.A., Australia, 6000</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>3</month>
<year>1975</year>
</pub-date>
<volume>40</volume>
<issue>309</issue>
<fpage>65</fpage>
<lpage>69</lpage>
<history>
<date date-type="received">
<day>17</day>
<month>4</month>
<year>1974</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1975, The Mineralogical Society</copyright-statement>
<copyright-year>1975</copyright-year>
<abstract>
<title>Summary</title>
<p>The garnierite, which occurs in the oxide zone overlying a nickel sulphide deposit, consists of talc-like and serpentine-like components, with the former predominating. Chemical and electron-probe analyses give NiO contents ranging between 39&#x00B7;6 and 43&#x00B7;9 weight %.</p></abstract>
</article-meta>
</front>
</article>
