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<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.1973.039.303.10</article-id>
<title-group>
<article-title>The Kabo, Nigeria, Meteorite Fall</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Hutchison</surname>
<given-names>R.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Ajakaiye</surname>
<given-names>D. E.</given-names>
</name>
<xref ref-type="author-notes" rid="FN1">1</xref></contrib>
<contrib contrib-type="author">
<name>
<surname>Elliott</surname>
<given-names>C. J.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Fry</surname>
<given-names>F. A.</given-names>
</name>
<xref ref-type="author-notes" rid="FN2">2</xref></contrib>
<aff>Department of Mineralogy, British Museum (Natural History), Cromwell Road, London SW7 5BD</aff></contrib-group>
<author-notes>
<fn fn-type="current-aff" id="FN1"><label>1</label><p>Department of Physics, Ahmadu Bello University, Zaria, Nigeria.</p></fn>
<fn fn-type="current-aff" id="FN2"><label>2</label><p>Health Physics and Medical Division, A.E.R.E. Harwell, Berks., England.</p></fn></author-notes>
<pub-date pub-type="ppub">
<month>9</month>
<year>1973</year>
</pub-date>
<volume>39</volume>
<issue>303</issue>
<fpage>340</fpage>
<lpage>345</lpage>
<history>
<date date-type="received">
<day>5</day>
<month>12</month>
<year>1972</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1973, The Mineralogical Society</copyright-statement>
<copyright-year>1973</copyright-year>
<abstract>
<title>Summary</title>
<p>At least four stones fell over a distance of about 9 km at the end of a west to east trajectory on 25 April 1971 at about 1630 hours local time. Their approximate location is 11&#x00B0; 51&#x2032; N., 8&#x00B0; 13&#x2032; E. About 13&#x00B7;4 kg of this xenolithic bronzite chondrite, class H<sub>4</sub>, were recovered. A bulk chemical analysis with total Fe = 29&#x00B0;4 % (wt), is presented. Olivine is Fa<sub>18.9</sub> (molec.) in composition. Concentrations of the cosmogenic radionuclides <sup>22</sup>Na, <sup>26</sup>Al, and <sup>54</sup>Mn were 71&#x00B1;6, 56&#x00B1;5 and 84&#x00B1;6 dpm/kg, respectively.</p></abstract>
</article-meta>
</front>
</article>
