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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.1969.037.285.06</article-id>
<title-group>
<article-title>Further Detail on the Crystal Structure of Zussmanitc</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Lopes-Vieira</surname>
<given-names>A.</given-names>
</name>
<xref ref-type="author-notes" rid="FN1">1</xref></contrib>
<contrib contrib-type="author">
<name>
<surname>Zussman</surname>
<given-names>J.</given-names>
</name>
<xref ref-type="author-notes" rid="FN2">2</xref></contrib>
<aff>Department of Geology and Mineralogy, Parks Road, Oxford</aff></contrib-group>
<author-notes>
<fn fn-type="present-address" id="FN1"><label>1</label><p>Now at Lab. de Technicas Fisico-Quimicas, Junta de Invest. do Ultramar, Alameda D. Alf. Henriques, 41-4 Esq. Lisbon, Portugal.</p></fn>
<fn fn-type="present-address" id="FN2"><label>2</label><p>Now at the Department of Geology, The University, Manchester 13, England.</p></fn></author-notes>
<pub-date pub-type="ppub">
<month>3</month>
<year>1969</year>
</pub-date>
<volume>37</volume>
<issue>285</issue>
<fpage>49</fpage>
<lpage>60</lpage>
<history>
<date date-type="received">
<day>14</day>
<month>6</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>Mineral data and a brief outline of the structure for zussmanite (ideal formula KFe<sub>13</sub>Si<sub>17</sub>AlO<sub>42</sub>(OH)<sub>14</sub>)have been published previously. This paper describes the determination of the crystal structure and presents and discusses the results. The structure consists of rhombohedrally stacked layers of Fe-(O,OH) octahedra to each side of which are attached rings of six (Si,Al)-O tetrahedra. These composite layers are linked to one another by rings of three (Si,Al)-O tetrahedra, and by potassium atoms, the latter in positions analogous to those in a mica. There is some evidence of disorder of the layer stacking. Interatomic distances and angles, and valency balance, are discussed.</p></abstract>
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