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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.1938.025.163.04</article-id>
<title-group>
<article-title>An X-Ray Examination of Mordenite (Ptilolite)</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Waymouth</surname>
<given-names>C.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Thornely</surname>
<given-names>P. C.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Taylor</surname>
<given-names>W. H.</given-names>
</name></contrib>
<aff>Physics Department, College of Technology, Manchester</aff></contrib-group>
<pub-date pub-type="ppub">
<month>12</month>
<year>1938</year>
</pub-date>
<volume>25</volume>
<issue>163</issue>
<fpage>212</fpage>
<lpage>216</lpage>
<copyright-statement>Copyright &#x00A9; 1938, The Mineralogical Society</copyright-statement>
<copyright-year>1938</copyright-year>
<abstract>
<title>IV. Summary</title>
<p>Specimens of the fibrous zeolite mordenite (ptilolite) have been examined by X-ray methods, and the specific gravity and pyroelectric properties determined. Laue and oscillation photographs indicate that the structure possesses orthorhombic symmetry, and the unit cell, with edges <italic>a</italic> 18&#x00B7;25, <italic>b</italic> 20&#x00B7;35, <italic>c</italic> 7&#x00B7;50 &#x00C5;., contains four molecules of composition (Ca,Na<sub>2</sub>,K<sub>2</sub>)Al<sub>2</sub>Si<sub>10</sub>O<sub>24</sub>.7H<sub>2</sub>O. The space-group is either <inline-formula><mml:math><mml:mrow><mml:msubsup><mml:mrow><mml:mi>D</mml:mi></mml:mrow><mml:mrow><mml:mn>2</mml:mn><mml:mi>h</mml:mi></mml:mrow><mml:mrow><mml:mn>17</mml:mn></mml:mrow></mml:msubsup><mml:mo>&#x003D;</mml:mo><mml:mtext>Cmcm</mml:mtext></mml:mrow></mml:math></inline-formula> or <inline-formula><mml:math><mml:mrow><mml:msubsup><mml:mrow><mml:mi>C</mml:mi></mml:mrow><mml:mrow><mml:mn>2</mml:mn><mml:mi>v</mml:mi></mml:mrow><mml:mrow><mml:mn>12</mml:mn></mml:mrow></mml:msubsup><mml:mo>&#x003D;</mml:mo><mml:mtext>Cmc</mml:mtext></mml:mrow></mml:math></inline-formula>; the pyroelectric tests are somewhat inconclusive, but indicate that the <italic>c</italic>-axis [001] is probably polar. The structure is probably based on a framework of linked tetrahedra.</p>
</abstract>
</article-meta>
</front>
</article>
