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<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.1972.038.298.06</article-id>
<title-group>
<article-title>The Crystal Structure of Stilpnomelane. Part II. The Full Cell</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Eggleton</surname>
<given-names>R. A.</given-names>
</name>
<aff>Department of Geology, Australian National University, Canberra, A.C.T., Australia</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>6</month>
<year>1972</year>
</pub-date>
<volume>38</volume>
<issue>298</issue>
<fpage>693</fpage>
<lpage>711</lpage>
<history>
<date date-type="received">
<day>11</day>
<month>3</month>
<year>1971</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1972, The Mineralogical Society</copyright-statement>
<copyright-year>1972</copyright-year>
<abstract>
<title>Summary</title>
<p>The structural formula of stilpnomelane averaged from 37 representative literature analyses and based on the determined structure is (Ca,Na,K)<sub>4</sub>(Ti<sub>0&#x00B7;1</sub>Al<sub>2&#x00B7;3</sub>Fe<sub>35&#x00B7;5</sub>Mn<sub>0&#x00B7;8</sub>Mg<sub>9&#x00B7;3</sub>)[Si<sub>63</sub>Al<sub>9</sub>](O,OH)<sub>216</sub>&#x00B7;<italic>n</italic>H<sub>2</sub>O. Ferrostilpnomelanes have up to 12 <italic>R</italic><sup>3+</sup> cations in the octahedral sheet, ferristilpnomelanes commonly have between 24 and 30 <italic>R</italic><sup>3+</sup> cations, rarely up to 37. The two groups can be distinguished by accurate X-ray powder diffraction, ferrostilpnomelanes having <italic>d</italic><sub>001</sub> less and <italic>a</italic> greater than have ferristilpnomelanes. The unit cell is triclinic, <italic>a</italic> = <italic>b</italic>&#x223C;21&#x00B7;8 &#x00C5;, <italic>&#x03B3;</italic> = 120&#x00B0;, <italic>d</italic><sub>001</sub>&#x223C;12&#x00B7;2 &#x00C5;, <inline-formula><mml:math><mml:mrow><mml:mi>P</mml:mi><mml:mover><mml:mi>I</mml:mi><mml:mo>&#x00AF;</mml:mo></mml:mover></mml:mrow></mml:math></inline-formula> Hexagonal groups or &#x2018;islands&#x2019; of 24 silicon-oxygen tetrahedra co-ordinate to the octahedral sheet, the centres of the &#x2018;islands&#x2019; are displaced by 5<italic>a</italic>/12, 8<italic>b</italic>/12 on either side of the octahedral sheet as a result of warping of this sheet to permit articulation with the smaller tetrahedral sheet. The 24-tetrahedra &#x2018;islands&#x2019; are linked laterally by 6-member rings of inverted tetrahedra, which in turn link at their apices to like rings connecting the next sheet of &#x2018;islands&#x2019;. Thus a single tetrahedral layer is 4 tetrahedra thick and has symmetry 6/<italic>m</italic>. The 6-member rings of tetrahedra act as hinges permitting up to 0&#x00B7;5 &#x00C5; extension or contraction of the tetrahedral sheet to accommodate variations in the octahedral sheet dimensions with varying <italic>R</italic><sup>2+</sup>/<italic>R</italic><sup>3+</sup> ratio.</p></abstract>
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