<?xml version="1.0"?>
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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.1986.050.357.14</article-id>
<article-categories>
<subj-group>
<subject>Mineralogy</subject>
</subj-group>
</article-categories>
<title-group>
<article-title>Synthetic Mn-Kilchoanite&#x2014;A New Development in Polymorphism of Melilite</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Kimata</surname>
<given-names>Mitsuyoshi</given-names>
</name>
<aff>Institute of Geoscience, the University of Tsukuba, Ibaraki 305, Japan</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>9</month>
<year>1986</year>
</pub-date>
<volume>50</volume>
<issue>357</issue>
<fpage>511</fpage>
<lpage>515</lpage>
<history>
<date date-type="received">
<day>1</day>
<month>8</month>
<year>1985</year>
</date>
<date date-type="rev-recd">
<day>2</day>
<month>1</month>
<year>1986</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1986, The Mineralogical Society</copyright-statement>
<copyright-year>1986</copyright-year>
<abstract>
<title>Abstract</title>
<p>Two compounds with the chemical composition Ca<sub>2.32</sub>Mn<sub>0.68</sub>Si<sub>2.00</sub>O<sub>7</sub> were synthesized from a molten carbonating silicate with the melilite composition. The synthetic samples were subsequently characterized by X-ray powder diffraction, IR absorption and EPMA, and they proved to be the anhydrous phases <italic>isomorphous</italic> with kilchoanite Ca<sub>3</sub>Si<sub>2</sub>O<sub>7</sub> and &#x00E5;kermanite Ca<sub>2</sub>MgSi<sub>2</sub>O<sub>7</sub> respectively, and to be polymorphous with each other. Their crystallochemical properties suggest that Mn-&#x00E5;kermanite is a high-temperature structure type of Mn-kilchoanite. Substitution of Mn<sup>2+</sup> with an intermediate ionic radius between those of Mg<sup>2+</sup> and Ca<sup>2+</sup> cations establishes the polymorphic relationship between &#x00E5;kermanite Ca<sub>2</sub>MgSi<sub>2</sub>O<sub>7</sub> and kilchoanite Ca<sub>3</sub>Si<sub>2</sub>O<sub>7</sub>.</p></abstract>
<kwd-group>
<title>Keywords</title>
<kwd>kilchoanite</kwd>
<kwd>&#x00E5;kermanite</kwd>
<kwd>manganese</kwd>
</kwd-group>
</article-meta>
</front>
</article>
