<?xml version="1.0"?>
<!DOCTYPE article SYSTEM "journalpublishing.dtd">
<article article-type="rapid-communication">
<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.1992.056.382.11</article-id>
<article-categories>
<subj-group>
<subject>Short Communications</subject>
</subj-group>
</article-categories>
<title-group>
<article-title>Ba Partitioning and the Origin of Anorthoclase Megacrysts in Basalitic Rocks</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Guo</surname>
<given-names>J. F.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Green</surname>
<given-names>T. H.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>O'Reilly</surname>
<given-names>S. Y.</given-names>
</name></contrib>
<aff>School of Earth Sciences, Macquarie University, Sydney, NSW 2109, Australia</aff></contrib-group>
<pub-date pub-type="ppub">
<month>3</month>
<year>1992</year>
</pub-date>
<volume>56</volume>
<issue>382</issue>
<fpage>101</fpage>
<lpage>107</lpage>
<history>
<date date-type="received">
<day>30</day>
<month>11</month>
<year>1990</year>
</date>
<date date-type="rev-recd">
<day>11</day>
<month>7</month>
<year>1991</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1992, The Mineralogical Society</copyright-statement>
<copyright-year>1992</copyright-year>
<kwd-group>
<title>Keywords</title>
<kwd>Ba</kwd>
<kwd>partition coefficient</kwd>
<kwd>anorthoclase</kwd>
<kwd>basalt</kwd>
<kwd>megacrysts</kwd>
</kwd-group>
</article-meta>
</front>
</article>
