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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.1975.040.312.09</article-id>
<title-group>
<article-title>Synthesis of K<sub>2</sub>SiSi<sub>3</sub>O<sub>9</sub> with Silicon in 4- and 6-Coordination</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Kinomura</surname>
<given-names>N.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Kume</surname>
<given-names>S.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Koizumi</surname>
<given-names>M.</given-names>
</name></contrib>
<aff>College of General Education and Institute of Scientific and Industrial Research, Osaka University, Toyonaka, 560, Japan</aff></contrib-group>
<pub-date pub-type="ppub">
<month>12</month>
<year>1975</year>
</pub-date>
<volume>40</volume>
<issue>312</issue>
<fpage>401</fpage>
<lpage>404</lpage>
<history>
<date date-type="received">
<day>16</day>
<month>9</month>
<year>1974</year>
</date>
<date date-type="rev-recd">
<day>18</day>
<month>12</month>
<year>1974</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1975, The Mineralogical Society</copyright-statement>
<copyright-year>1975</copyright-year>
<abstract>
<title>Summary</title>
<p>Two kinds of vitreous material with composition K<sub>2</sub>GeSi<sub>3</sub>O<sub>9</sub> and K<sub>2</sub>Si<sub>4</sub>O<sub>9</sub> were treated under conditions of high temperature and pressure. The X-ray diffraction patterns of the products were similar to that of K<sub>2</sub>TiSi<sub>3</sub>O<sub>9</sub>, which has the wadeite, K<sub>2</sub>ZrSi<sub>3</sub>O<sub>9</sub>, structure.</p>
<p>A natural crystal of K-feldspar was also treated under the same conditions. The product was found to consist of three phases, coesite, kyanite, and the above-mentioned K<sub>2</sub>Si<sub>4</sub>O<sub>9</sub>. Since Zr ions in wadeite are in a 6-coordinated site, one-quarter of Si ions in K<sub>2</sub>Si<sub>4</sub>O<sub>9</sub> are considered to be in 6-coordination. This is the first silicate in which Si ions occupy sites of 4- and 6-coordinations in one crystal at the same time.</p></abstract>
</article-meta>
</front>
</article>
