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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.1956.031.234.02</article-id>
<title-group>
<article-title>Determination of the Composition of Kalsilites by an X-ray Method</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Sahama</surname>
<given-names>Th. G.</given-names>
</name>
<aff>Professor of Geochemistry, Institute of Geology, Helsinki, Finland</aff></contrib>
<contrib contrib-type="author">
<name>
<surname>Neuvonen</surname>
<given-names>K. J.</given-names>
</name> <degrees>Ph.D.</degrees>
<aff>Geological Survey, Helsinki, Finland</aff></contrib>
<contrib contrib-type="author">
<name>
<surname>Hyt&#x00F6;nen</surname>
<given-names>Kai</given-names>
</name> <degrees>M.A.</degrees>
<aff>Institute of Geology, Helsinki, Finland</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>9</month>
<year>1956</year>
</pub-date>
<volume>31</volume>
<issue>234</issue>
<fpage>200</fpage>
<lpage>208</lpage>
<copyright-statement>Copyright &#x00A9; 1956, The Mineralogical Society</copyright-statement>
<copyright-year>1956</copyright-year>
<abstract>
<title>Summary</title>
<p>Three new analyses of kalsilite are given, with optical and X-ray data; two (K/(K + Na) = 0&#x00B7;95. 0&#x00B7;98) are from rocks where it is closely associated with nepheline. An analysis of one of the nephelines is also given (K/(K + Na) = 0&#x00B7;31). The cell dimensions vary appreciably with sodium content, and the composition of kalsilite may be determined from the equation: 100 K/(K + Na) = 100&#x2212;227&#x00B7;27(&#x0394; 6&#x00B7;264), where &#x0394; is the difference, in degrees, between the diffraction angles 2<italic>&#x03D1;</italic> for <inline-formula><mml:math><mml:mrow><mml:mn>10</mml:mn><mml:mover><mml:mi>1</mml:mi><mml:mo>&#x00AF;</mml:mo></mml:mover><mml:mn>2</mml:mn></mml:mrow></mml:math></inline-formula> and <inline-formula><mml:math><mml:mrow><mml:mn>10</mml:mn><mml:mover><mml:mi>1</mml:mi><mml:mo>&#x00AF;</mml:mo></mml:mover><mml:mn>1</mml:mn></mml:mrow></mml:math></inline-formula>, using Cu-<italic>K</italic>&#x03B1; radiation.</p></abstract>
</article-meta>
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