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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.1978.042.321.12</article-id>
<title-group>
<article-title>Hydrous Cordierite with Isotopically Light Oxygen from Granulites, Strangways Range, Central Australia</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Wilson</surname>
<given-names>Allan F.</given-names>
</name>
<aff>Department of Geology and Mineralogy, University of Queensland, St. Lucia (Brisbane), Queensland, Australia, 4067</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>3</month>
<year>1978</year>
</pub-date>
<volume>42</volume>
<issue>321</issue>
<fpage>89</fpage>
<lpage>92</lpage>
<history>
<date date-type="received">
<day>13</day>
<month>12</month>
<year>1976</year>
</date>
<date date-type="rev-recd">
<day>16</day>
<month>6</month>
<year>1977</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1978, The Mineralogical Society</copyright-statement>
<copyright-year>1978</copyright-year>
<abstract>
<title>Summary</title>
<p>Two new analyses of magnesian cordierites (MgO &#x223C; 12 %) reveal about 1% by weight of H<sub>2</sub>O +, and one sample contains 15 &#x00D7; 10<sup>&#x2212;5</sup> cm<sup>3</sup>STP/gm argon, which is twenty times in excess of argon expected for its age. Host granulites contain unexpectedly light oxygen, and three cordierites have &#x03B4; <sup>18</sup>O values of 2&#x00B7;0, 2&#x00B7;8, and 3&#x00B7;1 &#x2030;, respectively.</p></abstract>
</article-meta>
</front>
</article>
