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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.1973.039.303.05</article-id>
<title-group>
<article-title>Lithium-Aluminium Micas from the Meldon Aplite, Devonshire, England</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Chaudhry</surname>
<given-names>M. Nawaz</given-names>
</name>
<xref ref-type="author-notes" rid="FN1">1</xref></contrib>
<contrib contrib-type="author">
<name>
<surname>Howie</surname>
<given-names>R. A.</given-names>
</name></contrib>
<aff>Department of Geology, King's College, University of London</aff></contrib-group>
<author-notes>
<fn fn-type="present-address" id="FN1"><label>1</label><p>Present address: Department of Geology, University of the Panjab, Lahore, Pakistan.</p></fn></author-notes>
<pub-date pub-type="ppub">
<month>9</month>
<year>1973</year>
</pub-date>
<volume>39</volume>
<issue>303</issue>
<fpage>289</fpage>
<lpage>296</lpage>
<history>
<date date-type="received">
<day>15</day>
<month>11</month>
<year>1972</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1973, The Mineralogical Society</copyright-statement>
<copyright-year>1973</copyright-year>
<abstract>
<title>Summary</title>
<p>Chemical analyses of sixteen lithium-aluminium micas are presented along with their optical, physical, and X-ray data. Compositional variation, substitution relations in structural positions, and octahedral occupancy are discussed. The 2M<sub>2</sub> structural types are found to crystallize in volatilerich low-temperature environments whereas the 1M polytypes occur in comparatively volatile-poor and higher-temperature environments. Variation diagrams have been constructed to show the relationship between octahedral sites occupied by (Fe<sup>2+</sup>+ Fe<sup>3+</sup>+<inline-formula><mml:math><mml:mrow><mml:mstyle scriptlevel='+1'><mml:mfrac><mml:mn>1</mml:mn><mml:mn>3</mml:mn></mml:mfrac></mml:mstyle></mml:mrow></mml:math></inline-formula>Mn+Ti) and refractive indices and specific gravities.</p></abstract>
</article-meta>
</front>
</article>
