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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.1976.040.313.03</article-id>
<title-group>
<article-title>Nickeloan Pyroaurite from Leslie, Aberdeenshire</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Wilson</surname>
<given-names>M. J.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Cradwick</surname>
<given-names>P. D.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Berrow</surname>
<given-names>M. L.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>McHardy</surname>
<given-names>W. J.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Russell</surname>
<given-names>J. D.</given-names>
</name></contrib>
<aff>The Macaulay Institute for Soil Research, Craigiebuckler, Aberdeen AB9 2QJ</aff></contrib-group>
<pub-date pub-type="ppub">
<month>3</month>
<year>1976</year>
</pub-date>
<volume>40</volume>
<issue>313</issue>
<fpage>447</fpage>
<lpage>451</lpage>
<history>
<date date-type="received">
<day>1</day>
<month>4</month>
<year>1975</year>
</date>
<date date-type="rev-recd">
<day>21</day>
<month>4</month>
<year>1975</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1976, The Mineralogical Society</copyright-statement>
<copyright-year>1976</copyright-year>
<abstract>
<title>Summary</title>
<p>A nickel-bearing mineral belonging to the pyroaurite-sj&#x00F6;grenite group has been found in a serpentinite rock near the village of Leslie, Aberdeenshire. X-ray powder diffraction data and electron-probe microanalysis indicate that the mineral has a three-layer rhombohedral structure with a probable formula near <inline-formula><mml:math><mml:mrow><mml:msubsup><mml:mrow><mml:mi>Mg</mml:mi></mml:mrow><mml:mrow><mml:mn>4</mml:mn></mml:mrow><mml:mrow><mml:mn>2</mml:mn><mml:mo>&#x002B;</mml:mo></mml:mrow></mml:msubsup><mml:msubsup><mml:mrow><mml:mi>Ni</mml:mi></mml:mrow><mml:mrow><mml:mn>2</mml:mn></mml:mrow><mml:mrow><mml:mn>2</mml:mn><mml:mo>&#x002B;</mml:mo></mml:mrow></mml:msubsup><mml:msubsup><mml:mrow><mml:mi>Fe</mml:mi></mml:mrow><mml:mrow><mml:mn>2</mml:mn></mml:mrow><mml:mrow><mml:mn>3</mml:mn><mml:mo>&#x002B;</mml:mo></mml:mrow></mml:msubsup><mml:msub><mml:mrow><mml:mo>(</mml:mo><mml:mi>OH</mml:mi><mml:mo>)</mml:mo></mml:mrow><mml:mn>13</mml:mn></mml:msub><mml:msub><mml:mi>CO</mml:mi><mml:mn>3</mml:mn></mml:msub><mml:mo>&#x00B7;</mml:mo><mml:mn>4</mml:mn><mml:msub><mml:mi>H</mml:mi><mml:mn>2</mml:mn></mml:msub><mml:mi>O</mml:mi></mml:mrow></mml:math></inline-formula>. The mineral can therefore be described as nickeloan pyroaurite. It decomposes readily in mildly acid conditions and if inherited by serpentinite-derived soils could well be an important source of plant-available nickel.</p></abstract>
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