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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.1923.020.103.03</article-id>
<title-group>
<article-title>On the Occurrence of Petalite and Pneumatolytic Apatite in the Meldon Aplite, Okehampton, Devonshire<xref ref-type="author-notes" rid="FN1">1</xref></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>McLintock</surname>
<given-names>W. F. P.</given-names>
</name><degrees>D.Sc., F.G.S.</degrees>
<aff>Curator, Museum of Practical Geology, London</aff></contrib></contrib-group>
<author-notes>
<fn fn-type="com" id="FN1"><label>1</label><p>Communicated by permission of the Director, H.M. Geological Survey.</p></fn></author-notes>
<pub-date pub-type="ppub">
<month>12</month>
<year>1923</year>
</pub-date>
<volume>20</volume>
<issue>103</issue>
<fpage>140</fpage>
<lpage>150</lpage>
<copyright-statement>Copyright &#x00A9; 1923, The Mineralogical Society</copyright-statement>
<copyright-year>1923</copyright-year>
<abstract>
<title>Summary</title>
<p>(1) Certain portions of the aplite have developed a soda-lithia phase characterized by the presence of petalite, a mineral not previously recorded from the British Isles, and its product of decomposition, montmorillonite.</p>
<p>(2) The Meldon aplite affords a good example of the pneumatolytic phenomena so characteristic of the granites of the West of England.</p>
<p>(3) Evidence is brought forward to show that apatite occurs as a pneumatolytic mineral in the aplite.</p>
<p>I desire to express my most cordial thanks to Dr. E. H Young of Okehampton, who placed his material and knowledge of the district entirely at my disposal for the purposes of this investigation.</p></abstract>
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