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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.1967.036.278.10</article-id>
<title-group>
<article-title>X-Ray Data on Some Calcium-Iron-Oxygen Compounds</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Hughes</surname>
<given-names>H.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Roos</surname>
<given-names>P.</given-names>
</name>
<xref ref-type="author-notes" rid="FN1">1</xref></contrib>
<contrib contrib-type="author">
<name>
<surname>Goldring</surname>
<given-names>D. C.</given-names>
</name></contrib>
<aff>United Steel Cos. Ltd., Research &#x0026; Development Department, Swinden Laboratories, Moorgate, Rotherham</aff></contrib-group>
<author-notes>
<fn fn-type="present-address" id="FN1"><label>1</label><p>Now at Technische Hogeschool, Delft, Holland.</p></fn></author-notes>
<pub-date pub-type="ppub">
<month>6</month>
<year>1967</year>
</pub-date>
<volume>36</volume>
<issue>278</issue>
<fpage>280</fpage>
<lpage>291</lpage>
<history>
<date date-type="received">
<day>28</day>
<month>11</month>
<year>1966</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1967, The Mineralogical Society</copyright-statement><copyright-year>1967</copyright-year><abstract><title>Summary</title><p>Synthetic mixtures of CaO and Fe<sub>2</sub>O<sub>3</sub> fired in air at temperatures in the range 1180&#x00B0; C to 1240&#x00B0; C in some cases lost oxygen and formed ferrous-iron-bearing compounds. Samples after firing were examined by incident light microscopy and X-ray diffraction; new powder data are presented for the phases reported. In addition to <italic>&#x03B1;</italic>-Fe<sub>2</sub>O<sub>3</sub>, CaFe<sub>2</sub>O<sub>4</sub>, and Ca<sub>2</sub>Fe<sub>2</sub>O<sub>53</sub>. four distinct phases have been identified. These are <inline-formula><mml:math><mml:mrow><mml:msubsup><mml:mrow><mml:mtext>CaFe</mml:mtext></mml:mrow><mml:mrow><mml:mn>4</mml:mn></mml:mrow><mml:mrow><mml:mo>&#x2034;</mml:mo></mml:mrow></mml:msubsup><mml:msub><mml:mi>O</mml:mi><mml:mn>7</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>,<inline-formula><mml:math><mml:mrow><mml:msub><mml:mi>Ca</mml:mi><mml:mrow><mml:mn>7</mml:mn><mml:mo>&#x00B7;</mml:mo><mml:mn>2</mml:mn></mml:mrow></mml:msub><mml:msubsup><mml:mrow><mml:mi>Fe</mml:mi></mml:mrow><mml:mrow><mml:mn>0</mml:mn><mml:mo>&#x00B7;</mml:mo><mml:mn>8</mml:mn></mml:mrow><mml:mrow><mml:mo>&#x2033;</mml:mo></mml:mrow></mml:msubsup><mml:msubsup><mml:mrow><mml:mi>Fe</mml:mi></mml:mrow><mml:mrow><mml:mn>30</mml:mn></mml:mrow><mml:mrow><mml:mo>&#x2034;</mml:mo></mml:mrow></mml:msubsup><mml:msub><mml:mi>O</mml:mi><mml:mn>53</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>, and two forms of <inline-formula><mml:math><mml:mrow><mml:msub><mml:mrow><mml:mo>(</mml:mo><mml:mi>Ca</mml:mi><mml:mo>,</mml:mo><mml:msup><mml:mi>Fe</mml:mi><mml:mo>&#x2033;</mml:mo></mml:msup><mml:mo>,</mml:mo><mml:mi>Mg</mml:mi><mml:mo>)</mml:mo></mml:mrow><mml:mn>4</mml:mn></mml:msub><mml:msubsup><mml:mrow><mml:mi>Fe</mml:mi></mml:mrow><mml:mrow><mml:mn>14</mml:mn></mml:mrow><mml:mrow><mml:mo>&#x2034;</mml:mo></mml:mrow></mml:msubsup><mml:msub><mml:mi>O</mml:mi><mml:mn>25</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>, described previously by Braun and Kwestroo (1960). The likely compositions of these phases are given.</p></abstract>
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