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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.1987.051.360.09</article-id>
<title-group>
<article-title>The Composition and Distribution of Nodular Monazite in the Lower Palaeozoic Rocks of Great Britain</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Read</surname>
<given-names>D.</given-names>
</name>
<xref ref-type="author-notes" rid="FN1">*</xref>
<aff>University of Wales, Institute of Science and Technology, P.O. Box 13, Cardiff CF1 3XF</aff></contrib>
<contrib contrib-type="author">
<name>
<surname>Cooper</surname>
<given-names>D. C.</given-names>
</name>
<aff>British Geological Survey, Keyworth, Nottingham NG12 5GG</aff></contrib>
<contrib contrib-type="author">
<name>
<surname>McArthur</surname>
<given-names>J. M.</given-names>
</name>
<aff>University College London, Gower Street, London WC1E 6BT</aff></contrib></contrib-group>
<author-notes>
<fn fn-type="present-address" id="FN1"><label>*</label><p>Present address: W. S. Atkins and Partners, Longcross Court, Newport Road, Cardiff CF2 1AD.</p></fn></author-notes>
<pub-date pub-type="ppub">
<month>6</month>
<year>1987</year>
</pub-date>
<volume>51</volume>
<issue>360</issue>
<fpage>271</fpage>
<lpage>280</lpage>
<history>
<date date-type="received">
<day>22</day>
<month>11</month>
<year>1985</year>
</date>
<date date-type="rev-recd">
<day>3</day>
<month>6</month>
<year>1986</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1987, The Mineralogical Society</copyright-statement>
<copyright-year>1987</copyright-year>
<abstract>
<title>Abstract</title>
<p>Millimetric, ellipsoidal monazite nodules found within Lower Palaeozoic sedimentary rocks in Wales, south-west England and Brittany are characterised by a pronounced zonation of light and heavy <italic>REE</italic>, an inclusion fabric of low-grade metamorphic minerals indistinguishable from the host rock and a low Th content. They are interpreted as the product of <italic>in situ</italic> recrystallization of detrital monazites derived from pegmatitic or granitic source rocks and are potentially useful as indicators of Lower Palaeozoic sedimentary rock provenance.</p></abstract>
<kwd-group>
<title>Keywords</title>
<kwd>monazite</kwd>
<kwd>nodules</kwd>
<kwd>Lower Palaeozoic rocks</kwd>
<kwd>rare earth elements</kwd>
<kwd>Great Britain</kwd>
</kwd-group>
</article-meta>
</front>
</article>
