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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.1964.033.265.06</article-id>
<title-group>
<article-title>Some Orthopyroxenes from Scottish Metamorphic Rocks</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Howie</surname>
<given-names>R. A.</given-names>
</name><degrees>M.A., Ph.D., F.G.S.</degrees>
<aff>Department of Geology, King's College, London</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>6</month>
<year>1964</year>
</pub-date>
<volume>33</volume>
<issue>265</issue>
<fpage>903</fpage>
<lpage>911</lpage>
<copyright-statement>Copyright &#x00A9; 1964, The Mineralogical Society</copyright-statement>
<copyright-year>1964</copyright-year>
<abstract>
<title>Summary</title>
<p>Chemical analyses, cell parameters, and optical properties are presented for seven Scottish orthopyroxenes: four from Harris, two from Scourie, and one from Belhelvie, Aberdeenshire. The compositions range from En<sub>83&#x00B7;6</sub> to En<sub>55&#x00B7;5</sub>. Six of the orthopyroxenes are from pyroxene granulites or related rocks and the other is from a plagioclase-hypersthene hornfels: the latter mineral is notable in having 7&#x00B7;21% Al<sub>2</sub>O<sub>3</sub>, causing a considerable contraction in the <italic>a</italic> and <italic>b</italic> cell parameters. The alumina content of orthopyroxenes is briefly discussed. Analyses are also given for olivine and diopsidic augite from a South Harris ultrabasic gneiss and for two enderbitic pyroxene gneisses from Scourie.</p></abstract>
</article-meta>
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</article>
