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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.1969.037.287.04</article-id>
<title-group>
<article-title>Segregation and Cation-Ordering in Sj&#x00F6;grenite and Pyroaurite</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Taylor</surname>
<given-names>H. F. W.</given-names>
</name>
<aff>Department of Chemistry, University of Aberdeen, Old Aberdeen, Scotland</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>9</month>
<year>1969</year>
</pub-date>
<volume>37</volume>
<issue>287</issue>
<fpage>338</fpage>
<lpage>342</lpage>
<history>
<date date-type="received">
<day>30</day>
<month>12</month>
<year>1968</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1969, The Mineralogical Society</copyright-statement>
<copyright-year>1969</copyright-year>
<abstract>
<title>Summary</title>
<p>A specimen from L&#x00E5;ngban, Sweden, was found to consist largely of sj&#x00F6;grenite in which segregation and ordering of the metal cations had occurred, yielding an intergrowth of regions of two main types with compositions probably of or near Mg<sub>2/3</sub>Fe<sub>1/3</sub>(OH)<sub>2</sub>(CO<sub>3</sub>)<sub>1/6</sub>(H<sub>2</sub>O)<sub>0&#x00B7;4</sub> and Mg<sub>12/13</sub>Fe<sub>1/13</sub>(OH)<sub>2</sub>(CO<sub>3</sub>)<sub>1/26</sub>(H<sub>2</sub>O)<sub>0&#x00B7;8</sub>. To a smaller extent segregation had proceeded further, giving regions probably approximating to the end-member Mg(OH)<sub>2</sub>.H<sub>2</sub>O. It is suggested that the names sj&#x00F6;grenite and pyroaurite be used for the 2H- and 3R- polytypes of this structure irrespective of Mg:Fe ratio, segregation, or cation ordering.</p></abstract>
</article-meta>
</front>
</article>
