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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.1971.038.293.12</article-id>
<title-group>
<article-title>The Molteno Meteorite</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Frost</surname>
<given-names>Michael J.</given-names>
</name>
<xref ref-type="author-notes" rid="FN1">1</xref>
<aff>British Museum (Natural History), London, S.W. 7</aff></contrib></contrib-group>
<author-notes>
<fn fn-type="present-address" id="FN1"><label>1</label><p>Present address: Dept. of Geology, Northern Polytechnic, London, N. 7.</p></fn></author-notes>
<pub-date pub-type="ppub">
<month>3</month>
<year>1971</year>
</pub-date>
<volume>38</volume>
<issue>293</issue>
<fpage>89</fpage>
<lpage>93</lpage>
<history>
<date date-type="received">
<day>2</day>
<month>2</month>
<year>1968</year>
</date>
<date date-type="rev-recd">
<day>31</day>
<month>7</month>
<year>1969</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1971, The Mineralogical Society</copyright-statement>
<copyright-year>1971</copyright-year>
<abstract>
<title>Summary</title>
<p>The Molteno meteorite was seen to fall in South Africa in 1953. It is a howardite, with pyroxene varying from En<sub>76</sub>Fs<sub>22</sub>Wo<sub>2</sub> to En<sub>38</sub>Fs<sub>58</sub>Wo<sub>4</sub> and then to En<sub>33</sub>Fs<sub>26</sub>Wo<sub>41</sub>. Also present are twinned plagioclase (An 84&#x00B7;4%) and small quantities of olivine (Fa 12%), troilite, nickel-iron (Ni 4%), ilmenite, and an aluminian chromite with 0&#x00B7;71% V<sub>2</sub>O<sub>3</sub>. A bulk analysis and analyses of the metal, troilite, and combined silicates and oxides are given.</p></abstract>
</article-meta>
</front>
</article>
