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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">10.1180/002646198547567</article-id>
<title-group>
<article-title>Mineral Chemistry of a Peralkaline Combeite-lamprophyllite Nephelinite from Oldoinyo Lengai, Tanzania</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Dawson</surname>
<given-names>J. B.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Hill</surname>
<given-names>P. G.</given-names>
</name></contrib>
<aff>Department of Geology and Geophysics, University of Edinburgh, West Mains Road, Edinburgh EH9 3JW, UK</aff></contrib-group>
<pub-date pub-type="ppub">
<month>4</month>
<year>1998</year>
</pub-date>
<volume>62</volume>
<issue>2</issue>
<fpage>179</fpage>
<lpage>196</lpage>
<history>
<date date-type="received">
<day>15</day>
<month>4</month>
<year>1997</year>
</date>
<date date-type="rev-recd">
<day>26</day>
<month>8</month>
<year>1997</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1998, The Mineralogical Society</copyright-statement>
<copyright-year>1998</copyright-year>
<abstract>
<title>Abstract</title>
<p>A peralkaline nephelinite lava ([Na+K]/A1 2.15) from the active carbonatite volcano Oldoinyo Lengai, contains combeite, Ba lamprophyllite, a phase with affinities to delhayelite, CeSrNb perovskite, a CaNa phosphate high in Sr, Ba and K, and peralkaline glass; in addition to Fe-rich nepheline, aegirine-rich clinopyroxene and FeK-rich sodalite. The high alkali concentrations relative to almnina in the bulk rock could not have been achieved by fractionational crystallisation of the known Al-rich phenocryst phases (nepheline and sodalite) and some other process must be invoked.</p></abstract>
<kwd-group>
<title>Keywords</title>
<kwd>Oldoinyo Lengai</kwd>
<kwd>Tanzania</kwd>
<kwd>nephelinite</kwd>
<kwd>natrocarbonatite</kwd>
<kwd>combeite</kwd>
<kwd>Ba lamprophyllite</kwd>
<kwd>delhayelite</kwd>
<kwd>CaNa phosphate</kwd>
<kwd>peralkaline glasses</kwd>
</kwd-group>
</article-meta>
</front>
</article>
