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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.1980.043.331.01</article-id>
<title-group>
<article-title>Johnsomervilleite, a New Transition-Metal Phosphate Mineral from the Loch Quoich Area, Scotland</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Livingstone</surname>
<given-names>A.</given-names>
</name>
<aff>Department of Geology, Royal Scottish Museum, Chambers Street, Edinburgh EH1 1JF</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>9</month>
<year>1980</year>
</pub-date>
<volume>43</volume>
<issue>331</issue>
<fpage>833</fpage>
<lpage>836</lpage>
<history>
<date date-type="received">
<day>11</day>
<month>2</month>
<year>1980</year>
</date>
<date date-type="rev-recd">
<day>10</day>
<month>3</month>
<year>1980</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1980, The Mineralogical Society</copyright-statement>
<copyright-year>1980</copyright-year>
<abstract>
<title>Summary</title>
<p>Johnsomervilleite, Na<sub>10</sub>Ca<sub>6</sub>Mg<sub>18</sub>(Fe, Mn)<sub>25</sub> (PO<sub>4</sub>)<sub>36</sub> has Z = 3, <italic>a</italic> 15.00 &#x00C5;, <italic>c</italic> 42.75 &#x00C5; and cell volume 8330 &#x00C5;<sup>3</sup> and is a new rhombohedral species occurring in two metamorphic segregation pods in Moine gneiss of kyanite-sillimanite grade. Associated minerals are apatite, jahnsite, graftonite, mineral A, phosphosiderite, rockbridgeite, mitridatite, and vivianite. It is dark brown, brittle, and glassy, H = 4<inline-formula><mml:math><mml:mrow>
<mml:mstyle scriptlevel='+1'>
<mml:mfrac>
<mml:mn>1</mml:mn>
<mml:mn>2</mml:mn>
</mml:mfrac>
</mml:mstyle>
</mml:mrow>
</mml:math></inline-formula>, D = 3&#x00B7;35 (calc. 3.41) with a perfect basal (?) cleavage. Eight electron probe analyses are given and <italic>d</italic> spacings for 50 lines. The mineral, which is a Mg-Fe analogue of fillowite, is named after the late Mr J. M. Somerville who presented a specimen of garnet-quartz rock, which contained the new species, to the Royal Scottish Museum.</p></abstract>
</article-meta>
</front>
</article>
