<?xml version="1.0"?>
<!DOCTYPE article SYSTEM "journalpublishing.dtd">
<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.1975.040.312.03</article-id>
<title-group>
<article-title>A Sapphirine-Cordierite-Bronzite-Phlogopite Paragenesis from Namaqualand, South Africa</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Clifford</surname>
<given-names>T. N.</given-names>
</name>
<xref ref-type="aff" rid="A1">1</xref></contrib>
<contrib contrib-type="author">
<name>
<surname>Stumpfl</surname>
<given-names>E. F.</given-names>
</name>
<xref ref-type="aff" rid="A2">2</xref></contrib>
<contrib contrib-type="author">
<name>
<surname>McIver</surname>
<given-names>J. R.</given-names>
</name>
<xref ref-type="aff" rid="A1">1</xref></contrib></contrib-group>
<aff id="A1"><label>1</label>Department of Geology, University of the Witwatersrand, Johannesburg, South Africa</aff>
<aff id="A2"><label>2</label>Montanistische Hochschule, Leoben, Austria (formerly Mineralogisch-Petrographisches Institut, Universit&#x00E4;t Hamburg, Germany)</aff>
<pub-date pub-type="ppub">
<month>12</month>
<year>1975</year>
</pub-date>
<volume>40</volume>
<issue>312</issue>
<fpage>347</fpage>
<lpage>356</lpage>
<history>
<date date-type="received">
<day>6</day>
<month>9</month>
<year>1974</year>
</date>
<date date-type="rev-recd">
<day>9</day>
<month>12</month>
<year>1974</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1975, The Mineralogical Society</copyright-statement>
<copyright-year>1975</copyright-year>
<abstract>
<title>Summary</title>
<p>The rock composition and electron microprobe analyses of the five constituent minerals are presented for a sapphirine-cordierite-bronzite-phlogopite-spinel rock from Namaqualand, South Africa. These data are considered in relation to experimental data and the mineralogy of certain associated rock types, and it is suggested that the sapphirine-bearing rock represents a metamorphic residuum (restite) after extraction of anatectic granitic liquid from an original argillaceous sediment.</p></abstract>
</article-meta>
</front>
</article>
