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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.1981.044.334.14</article-id>
<title-group>
<article-title>The Composition of Solid Inclusions and the Occurrence of Shortite in Apatites from the Tororo Carbonatite Complex of Eastern Uganda</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Aspden</surname>
<given-names>J. A.</given-names>
</name>
<aff>Institute of Geological Sciences, Keyworth, Nottingham, England</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>6</month>
<year>1981</year>
</pub-date>
<volume>44</volume>
<issue>334</issue>
<fpage>201</fpage>
<lpage>204</lpage>
<history>
<date date-type="received">
<day>24</day>
<month>7</month>
<year>1980</year>
</date>
<date date-type="rev-recd">
<day>17</day>
<month>11</month>
<year>1980</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1981, The Mineralogical Society</copyright-statement>
<copyright-year>1981</copyright-year>
<abstract>
<title>Abstract</title>
<p>Apatite concentrates obtained from a carbonatite of the Tororo complex contain cogenetic fluid and solid primary inclusions. The solid inclusions are commonly composed of calcite and shortite and these minerals, together with the host apatite, were deposited from aqueous fluids at approximately 400 &#x00B0;C.</p></abstract>
</article-meta>
</front>
</article>
