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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.1965.035.271.06</article-id>
<title-group>
<article-title>The Mineralogy of the Potassium-Barium Feldspar Series I. The Determination of the Optical Properties of Natural Members</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Roy</surname>
<given-names>N. N.</given-names>
</name>
<aff>Department of Mineralogy and Petrology, Cambridge</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>9</month>
<year>1965</year>
</pub-date>
<volume>35</volume>
<issue>271</issue>
<fpage>508</fpage>
<lpage>518</lpage>
<history>
<date date-type="received">
<day>1</day>
<month>1</month>
<year>1965</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1965, The Mineralogical Society</copyright-statement>
<copyright-year>1965</copyright-year>
<abstract>
<title>Summary</title>
<p>Variation diagrams for the optic properties and densities of natural specimens within the series have been determined. They focus attention on two composition regions at about 45 % Cn and 65 % Cn. The significance of the first of these is uncertain, but it is suggested that the discontinuity at 65 % Cn is related to structural changes that take place at this composition.</p></abstract>
</article-meta>
</front>
</article>
