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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.1984.048.349.05</article-id>
<title-group>
<article-title>Unusual Sector Zoning in Lewisian Zircons</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Hoffman</surname>
<given-names>J. F.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Long</surname>
<given-names>J. V. P.</given-names>
</name></contrib>
<aff>Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge</aff></contrib-group>
<pub-date pub-type="ppub">
<month>12</month>
<year>1984</year>
</pub-date>
<volume>48</volume>
<issue>349</issue>
<fpage>513</fpage>
<lpage>517</lpage>
<history>
<date date-type="received">
<day>15</day>
<month>3</month>
<year>1983</year>
</date>
<date date-type="rev-recd">
<day>7</day>
<month>3</month>
<year>1984</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1984, The Mineralogical Society</copyright-statement>
<copyright-year>1984</copyright-year>
<abstract>
<title>Abstract</title>
<p>An unusual form of sector zoning has been recorded in some Lewisian zircons. The sectors lie in a plane cut perpendicular to the <italic>c</italic>-axis and are observed as variations in the intensity of cathodoluminescence, and in trace-element concentrations. Sectors radiating from the centre of growth out to the &#x007B;100&#x007D; faces exhibit low-intensity cathodoluminescence and are enriched in Y and depleted in Hf and Zr. Those radiating to the &#x007B;110&#x007D; faces are brightly luminescent, slightly enriched in Hf and depleted in Y. X-ray diffraction data, and comparison with previous studies of zircons, suggest that the sectors vary slightly in crystallographic orientation, such that the boundaries between sectors form discontinuities in the structure.</p></abstract>
</article-meta>
</front>
</article>
