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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.1981.044.334.18</article-id>
<title-group>
<article-title>Orientation and Geometry of the Thomsonite Unit Cell: A Re-Study</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Nawaz</surname>
<given-names>Rab</given-names>
</name>
<aff>Department of Geology, Ulster Museum</aff></contrib>
<contrib contrib-type="author">
<name>
<surname>Malone</surname>
<given-names>John F.</given-names>
</name>
<aff>Department of Chemistry, Queen's University, Belfast</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>6</month>
<year>1981</year>
</pub-date>
<volume>44</volume>
<issue>334</issue>
<fpage>231</fpage>
<lpage>234</lpage>
<history>
<date date-type="received">
<day>11</day>
<month>2</month>
<year>1980</year>
</date>
<date date-type="rev-recd">
<day>23</day>
<month>12</month>
<year>1980</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1981, The Mineralogical Society</copyright-statement>
<copyright-year>1981</copyright-year>
<abstract>
<title>Abstract</title>
<p>New X-ray and optical studies show that thomsonite has <italic>a</italic> &#x003C; <italic>b</italic> &#x003C; <italic>c</italic> and its optical orientation is <italic>&#x03B1;</italic> = <italic>b</italic>, <italic>&#x03B2;</italic> = <italic>c</italic>, and <italic>&#x03B3;</italic> = <italic>a</italic>. The refined cell dimensions of Old Kilpatrick thomsonite are <italic>a</italic> = 13.051, <italic>b</italic> = 13.092, and <italic>c</italic> = 13.263 &#x00C5;. The systematic absences <italic>h+l</italic> odd for <italic>h</italic>0<italic>l, h + k</italic> odd for  odd for <italic>hk</italic>0, and <italic>l</italic> odd for 0<italic>kl</italic> uniquely determine the space group as <italic>Pcnn</italic> for which the arrangement of the alumino-silicate framework is suggested. The exceptions to the above absences are the 704 reflection (due to Renninger effect) and many weak <italic>hk0</italic> reflections which suggest that the space group might be <italic>Pcnm or Pcn2</italic>. The observed habit, cleavage, and parallel growth are discussed in the light of the proposed framework structure.</p></abstract>
</article-meta>
</front>
</article>
