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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.1986.050.358.13</article-id>
<title-group>
<article-title>Pyroxenes and Coexisting Minerals in the Cheviot Granite</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Haslam</surname>
<given-names>H. W.</given-names>
</name>
<aff>British Geological Survey, 154 Clerkenwell Road, London EC1R 5DU</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>12</month>
<year>1986</year>
</pub-date>
<volume>50</volume>
<issue>358</issue>
<fpage>671</fpage>
<lpage>674</lpage>
<history>
<date date-type="received">
<day>31</day>
<month>1</month>
<year>1986</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1986, The Mineralogical Society</copyright-statement>
<copyright-year>1986</copyright-year>
<abstract>
<title>Abstract</title>
<p>Orthopyroxene and clinopyroxene, with biotite, are widespread in the high-level Cheviot granite, while amphibole is rare. The pyroxene compositions are very close to (Mg,Fe)<sub>2</sub>Si<sub>2</sub>O<sub>6</sub> and Ca(Mg,Fe)Si<sub>2</sub>O<sub>6</sub>. Biotite compositions, with low Si and Al, are characteristic of biotites coexisting with pyroxenes. Geothermometric estimates based on oxide and pyroxene compositions show that present mineral compositions result from post-consolidation equilibration.</p></abstract>
<kwd-group>
<title>Keywords</title>
<kwd>granite</kwd>
<kwd>Cheviot</kwd>
<kwd>rare earth elements</kwd>
<kwd>pyroxene</kwd>
<kwd>biotite</kwd>
<kwd>geothermometry</kwd>
</kwd-group>
</article-meta>
</front>
</article>
