<?xml version="1.0"?>
<!DOCTYPE article SYSTEM "journalpublishing.dtd">
<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.1965.034.268.36</article-id>
<title-group>
<article-title>Yellow Apophyllite from Korsn&#x00E4;s, Finland</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Sahama</surname>
<given-names>Th. G.</given-names>
</name>
<aff>University of Helsinki, Finland</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<year>1965</year>
</pub-date>
<volume>34</volume>
<issue>268</issue>
<fpage>406</fpage>
<lpage>415</lpage>
<copyright-statement>Copyright &#x00A9; 1965, The Mineralogical Society</copyright-statement>
<copyright-year>1965</copyright-year>
<abstract>
<title>Summary</title>
<p>The honey-yellow apophyllite from Korsn&#x00E4;s, Finland, for which chemical, optical, and X-ray data are given, shows a complex twinning. An inne penetration twin is surrounded by two outer penetration twins. The twin laws have been established. The prism faces of the complex crystal are not (100) as conven-tionally taken for apophyllitebut (520). The spacegroup <italic>P</italic>4/<italic>mnc</italic> commonly accepted for apophyllite could not be confirmed. It is suggested that the mineral is only pseudotetragonal, the true symmetry possibly being orthorhombic with space group <italic>Pnn2</italic> or <italic>Pnnm</italic>.</p></abstract>
</article-meta>
</front>
</article>
