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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.1973.039.303.03</article-id>
<title-group>
<article-title>The Crystal Structure of Julgoldite</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Allmann</surname>
<given-names>Rudolf</given-names>
</name>
<aff>Fachbereich Geowissenschaften, Philipps-Universit&#x00E4;t, 355 Marburg, Germany</aff></contrib>
<contrib contrib-type="author">
<name>
<surname>Donnay</surname>
<given-names>Gabrielle</given-names>
</name>
<aff>Department of Geological Sciences, McGill University, Montreal 101, Quebec, Canada</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>9</month>
<year>1973</year>
</pub-date>
<volume>39</volume>
<issue>303</issue>
<fpage>271</fpage>
<lpage>281</lpage>
<history>
<date date-type="received">
<day>2</day>
<month>10</month>
<year>1972</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1973, The Mineralogical Society</copyright-statement>
<copyright-year>1973</copyright-year>
<abstract>
<title>Summary</title>
<p>The structure of julgoldite, <inline-formula><mml:math><mml:mrow><mml:msub><mml:mi>Ca</mml:mi><mml:mn></mml:mn></mml:msub><mml:mrow><mml:mo>(</mml:mo><mml:msubsup><mml:mrow><mml:mi>Fe</mml:mi></mml:mrow><mml:mrow><mml:mn>1</mml:mn><mml:mo>&#x2212;</mml:mo><mml:mi>x</mml:mi></mml:mrow><mml:mrow><mml:mn>2</mml:mn><mml:mo>&#x002B;</mml:mo></mml:mrow></mml:msubsup><mml:msubsup><mml:mrow><mml:mi>Fe</mml:mi></mml:mrow><mml:mrow><mml:mi>x</mml:mi></mml:mrow><mml:mrow><mml:mn>3</mml:mn><mml:mo>&#x002B;</mml:mo></mml:mrow></mml:msubsup><mml:mo>)</mml:mo></mml:mrow><mml:msubsup><mml:mrow><mml:mi>Fe</mml:mi></mml:mrow><mml:mrow><mml:mn>2</mml:mn></mml:mrow><mml:mrow><mml:mn>3</mml:mn><mml:mo>&#x002B;</mml:mo></mml:mrow></mml:msubsup><mml:msub><mml:mi>Si</mml:mi><mml:mn>3</mml:mn></mml:msub><mml:msub><mml:mo>O</mml:mo><mml:mrow><mml:mn>10</mml:mn><mml:mo>&#x002B;</mml:mo><mml:mi>x</mml:mi></mml:mrow></mml:msub><mml:msub><mml:mi>(OH)</mml:mi><mml:mrow><mml:mn>4</mml:mn><mml:mo>&#x2212;</mml:mo><mml:mi>x</mml:mi></mml:mrow></mml:msub><mml:mrow><mml:mo>(</mml:mo><mml:mi>x</mml:mi><mml:mspace width="veryth:nmathspace"/><mml:mo>&#x2248;</mml:mo><mml:mspace width="veryth:nmathspace"/><mml:mn>0</mml:mn><mml:mo>&#x00B7;</mml:mo><mml:mn>5</mml:mn><mml:mo>)</mml:mo></mml:mrow></mml:mrow></mml:math></inline-formula>, has been determined and refined to an R value of 4&#x00B7;6 % based on 2417 symmetry-independent reflections, of which 765 are unobserved (weighted <italic>R</italic> = 4&#x00B7;3%). The cell dimensions are <italic>a</italic> 8&#x00B7;922(4), <italic>b</italic> 6&#x00B7;081(3), <italic>c</italic> 19&#x00B7;432(9) &#x00C5;, &#x03B2; 97&#x00B7;60(6)&#x00B0;, the space group is <italic>A2/m</italic> with <italic>Z</italic> = 4 and D<sub>cale</sub> 3&#x00B7;56 g cm<sup>&#x2212;3</sup>. Julgoldite is isostructural with pumpellyite; the Si-O and Ca-O distances of julgoldite are identical, within experimental accuracy, with corresponding distances in pumpellyite; the Fe-O distances of julgoldite are about 0&#x00B7;09 &#x00C5; longer than the corresponding (A1, Mg)-O distances in pumpellyite. The four hydroxyl groups and the extent of O-for-OH substitution are identified by valence-sum calculations.</p></abstract>
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</front>
</article>
