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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.1970.037.290.04</article-id>
<title-group>
<article-title>A Metallographic and Microprobe Study of the Metal Phases in the Weekeroo Station Meteorite</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Axon</surname>
<given-names>H. J.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Smith</surname>
<given-names>P. L.</given-names>
</name></contrib>
<aff>Metallurgy Department, The University, Manchester M13 9PL</aff></contrib-group>
<pub-date pub-type="ppub">
<month>6</month>
<year>1970</year>
</pub-date>
<volume>37</volume>
<issue>290</issue>
<fpage>670</fpage>
<lpage>673</lpage>
<history>
<date date-type="received">
<day>11</day>
<month>8</month>
<year>1969</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1970, The Mineralogical Society</copyright-statement>
<copyright-year>1970</copyright-year>
<abstract>
<title>Summary</title>
<p>The kamacite contains a general precipitation of micrometre-sized particles of exsolved taenite. Larger particles are found decorating Neumann lines and at kamacite grain boundaries. The coexisting kamacite and taenite appear to have nickel contents of 6&#x00B7;4 % and about 53%, which are consistent with a temperature of about 330&#x2013;60 &#x00B0;C on the binary iron-nickel equilibrium diagram.</p></abstract>
</article-meta>
</front>
</article>
