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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.1987.051.363.06</article-id>
<article-categories>
<subj-group subj-group-type="heading">
<subject>Mineralogy</subject>
</subj-group>
</article-categories>
<title-group>
<article-title>A New Natural Occurrence of Zirconolite (CaZrTi<sub>2</sub>O<sub>7</sub>) and Baddeleyite (ZrO<sub>2</sub>) in Basic Cumulates: The Laouni Layered Intrusion (Southern Hoggar, Algeria)</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Lorand</surname>
<given-names>J. P.</given-names>
</name>
<aff>Laboratoire de Min&#x00E9;ralogie du Museum National d'Histoire, Naturelle de Paris, Unit&#x00E9; associ&#x00E9;e au CNRS no. 286, 61 Rue Buffon, 75005 Paris, France</aff></contrib>
<contrib contrib-type="author">
<name>
<surname>Cottin</surname>
<given-names>J. Y.</given-names>
</name>
<aff>D&#x00E9;partment de G&#x00E9;ologie, IST Universit&#x00E9; d'Oran Essenia, Algeria</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>12</month>
<year>1987</year>
</pub-date>
<volume>51</volume>
<issue>363</issue>
<fpage>671</fpage>
<lpage>676</lpage>
<history>
<date date-type="received">
<day>24</day>
<month>11</month>
<year>1986</year>
</date>
<date date-type="rev-recd">
<day>5</day>
<month>2</month>
<year>1987</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1987, The Mineralogical Society</copyright-statement>
<copyright-year>1987</copyright-year>
<abstract>
<title>Abstract</title>
<p>Four grains of zirconolite and baddeleyite have been found in two plagioclase-rich adcumulates from the Laouni layered intrusion (Southern Hoggar, Algeria). Zirconolite is poor in <italic>REE</italic>; baddeleyite is chemically close to ZrO<sub>2</sub> and contains minor amounts of Hf. They are considered to be crystallization products of pockets of intercumulus liquid. The preferential distribution of zirconolite in anorthosite is explained in terms of expulsion of the intercumulus liquid by sintering or annealing of plagioclase. The crystallization of baddeleyite reflects the sharp increase of Zr in the trapped intercumulus liquid.</p></abstract>
<kwd-group>
<title>Keywords</title>
<kwd>zirconolite</kwd>
<kwd>baddeleyite</kwd>
<kwd>cumulate texture</kwd>
<kwd>Laouni</kwd>
<kwd>Hoggar</kwd>
<kwd>Algeria</kwd>
</kwd-group>
</article-meta>
</front>
</article>
