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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.1972.038.299.07</article-id>
<title-group>
<article-title>Talc-Kyanite-Quartz Schists and Other High-Pressure Assemblages from Zambia<xref ref-type="fn" rid="FN1">1</xref></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Vr&#x00E1;na</surname>
<given-names>S.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Barr</surname>
<given-names>M. W. C.</given-names>
</name>
<xref ref-type="author-notes" rid="FN2">2</xref>
<aff>Geological Survey Department, Lusaka, Zambia</aff></contrib></contrib-group>
<author-notes>
<fn fn-type="other" id="FN1"><label>1</label><p>Occasional Paper No. 48, published by permission of the Director, Geological Survey of Zambia.</p></fn>
<fn fn-type="present-address" id="FN2"><label>2</label><p>Present address: Dept. of Earth Sciences, The University, Leeds.</p></fn></author-notes>
<pub-date pub-type="ppub">
<month>9</month>
<year>1972</year>
</pub-date>
<volume>38</volume>
<issue>299</issue>
<fpage>837</fpage>
<lpage>846</lpage>
<history>
<date date-type="received">
<day>24</day>
<month>9</month>
<year>1971</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1972, The Mineralogical Society</copyright-statement>
<copyright-year>1972</copyright-year>
<abstract>
<title>Summary</title>
<p>Talc-kyanite-quartz schists, Mg-chlorite-kyanite-quartz schists, kyanite gedritites, and kyanite-bronzite gedritites occur in the Central Province of Zambia. Experimental work in the system MgO-Al<sub>2</sub>O<sub>3</sub>-SiO<sub>2</sub>-H<sub>2</sub>O suggests that these assemblages formed at pressures in excess of 10 kb.</p></abstract>
</article-meta>
</front>
</article>
