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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.1983.047.343.07</article-id>
<title-group>
<article-title>Crystal-Chemical Characterization of NaAlSiO<sub>4</sub> with the CaFe<sub>2</sub>O<sub>4</sub> Structure</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Yamada</surname>
<given-names>Hiroisa</given-names>
</name>
<xref ref-type="author-notes" rid="FN1">*</xref></contrib>
<contrib contrib-type="author">
<name>
<surname>Matsui</surname>
<given-names>Yoshito</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Ito</surname>
<given-names>Eiji</given-names>
</name></contrib>
<aff>Institute for Thermal Spring Research, Okayama University Misasa, Tottori-ken, 682-02, Japan</aff></contrib-group>
<author-notes>
<fn fn-type="present-address" id="FN1"><label>*</label><p>Present address: Department of Geology and Mineralogy, Faculty of Science, Kyoto University, Kyoto 606, Japan.</p></fn></author-notes>
<pub-date pub-type="ppub">
<month>6</month>
<year>1983</year>
</pub-date>
<volume>47</volume>
<issue>343</issue>
<fpage>177</fpage>
<lpage>181</lpage>
<history>
<date date-type="received">
<day>18</day>
<month>5</month>
<year>1982</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1983, The Mineralogical Society</copyright-statement>
<copyright-year>1983</copyright-year>
<abstract>
<title>Abstract</title>
<p>A high-pressure modification of NaAlSiO<sub>4</sub>, with the calcium ferrite structure was synthesized at pressures higher than 24 GPa using a double-stage split-sphere type high-pressure apparatus. The unit cell dimensions are: <italic>a</italic>=10.1546(8), <italic>b</italic>=8.6642(8), <italic>c</italic>= 2.7385(4) &#x00C5;, and <italic>V</italic> = 240.93(3) &#x00C5;<sup>3</sup> with the space group <italic>Pbnm</italic>. Calculated density is 3.916(1) g/cm<sup>3</sup>. The crystal structure was determined by the ordinary powder X-ray method. Both <italic>M</italic>1O<sub>6</sub> and <italic>M</italic>2O<sub>6</sub> octahedra run parallel to the <italic>c</italic>-axis, forming edge-shared double chains. The shared edges exhibit remarkable shortening (2.25&#x2013;2.39 &#x00C5;). Sodium atoms are located in the &#x2018;tunnel&#x2019; formed by the linked double chains, being in eightfold co-ordination. The structure is very similar to that predicted by Dempsey and Strens (1976) with the aid of the DLS method. The possible instability of the calcium ferrite type of Mg<sub>2</sub>SiO<sub>4</sub> is discussed.</p></abstract>
</article-meta>
</front>
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