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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.1982.045.337.29</article-id>
<title-group>
<article-title>The Pendennis Peralkaline Minette</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Hall</surname>
<given-names>A.</given-names>
</name>
<aff>Department of Geology, King's College, Strand, London WC2R 2LS</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<year>1982</year>
</pub-date>
<volume>45</volume>
<issue>337</issue>
<fpage>257</fpage>
<lpage>266</lpage>
<copyright-statement>Copyright &#x00A9; 1982, The Mineralogical Society</copyright-statement>
<copyright-year>1982</copyright-year>
<abstract>
<title>Abstract</title>
<p>The Pendennis minette has an exceptionally high K<sub>2</sub>O/Na<sub>2</sub>O ratio and is strongly peralkaline. Its constituent minerals, which are described in detail, are sanidine, biotite, two carbonates (dolomite and ferroan magnesite), two amphiboles (riebeckite and a new variety, potassium magnesio-arfvedsonite), and quartz. The major and trace dement composition of the minette indicates close affinities with the lamproitic lavas.</p></abstract>
</article-meta>
</front>
</article>
