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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.1973.039.302.08</article-id>
<title-group>
<article-title>The Barea, Dyarrl Island, and Emery Meteorites, and a Review of the Mesosiderites</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Mason</surname>
<given-names>Brian</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Jarosewich</surname>
<given-names>E.</given-names>
</name></contrib>
<aff>Smithsonian Institution, Washington, D.C., U.S.A.</aff></contrib-group>
<pub-date pub-type="ppub">
<month>6</month>
<year>1973</year>
</pub-date>
<volume>39</volume>
<issue>302</issue>
<fpage>204</fpage>
<lpage>215</lpage>
<history>
<date date-type="received">
<day>3</day>
<month>7</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>Barea and Emery are typical mesosiderites, whereas Dyarrl Island<xref ref-type="fn" rid="FN1">1</xref> is unique in having the lowest metal content and the highest FeO/(FeO + MgO) ratio of any meteorite of this class. Average pyroxene compositions have been determined for the individual mesosiderites, and show a sequential increase in FeSiO<sub>3</sub> content, ranging from a mean of 21 mole % for Veramin to 45 mole % for Dyarrl Island. Steinbach may possibly be classed as a mesosiderite, since its mineralogy is identical except for the absence of plagioclase. Dalgaranga and Mt. Padbury may be a paired fall. The chemical and mineralogical composition of the silicate material of the mesosiderites is similar to, but not identical with the howardites; the overall range of composition is greater in the mesosiderites.</p>
<p><fn fn-type="other" id="FN1"><label>1</label><p>The actual place of fall is Dyaul Island; see below.</p></fn></p></abstract>
</article-meta>
</front>
</article>
