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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.1989.053.372.05</article-id>
<article-categories>
<subj-group subj-group-type="heading">
<subject>Mineralogy</subject>
</subj-group>
</article-categories>
<title-group>
<article-title>Holtite, (Si<sub>2.25</sub>Sb<sub>0.75</sub>)B [Al<sub>6</sub>(Al<sub>0.43</sub>Ta<sub>0.27</sub>&#x25A1;<sub>0.30</sub>) O<sub>15</sub> (O,OH)<sub>2.25</sub>]: Crystal Structure and Crystal Chemistry</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Hoskins</surname>
<given-names>B. F.</given-names>
</name>
<aff>University of Melbourne, Parkville, Melbourne, Australia</aff></contrib>
<contrib contrib-type="author">
<name>
<surname>Mumme</surname>
<given-names>W. G.</given-names>
</name>
<aff>CSIRO, Division of Mineral Products, P.O. Box 124, Port Melbourne, Australia</aff></contrib>
<contrib contrib-type="author">
<name>
<surname>Pryce</surname>
<given-names>M. W.</given-names>
</name>
<aff>Government Chemical Laboratories, Perth, Western Australia</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>9</month>
<year>1989</year>
</pub-date>
<volume>53</volume>
<issue>372</issue>
<fpage>457</fpage>
<lpage>463</lpage>
<history>
<date date-type="received">
<day>30</day>
<month>9</month>
<year>1988</year>
</date>
<date date-type="rev-recd">
<day>13</day>
<month>1</month>
<year>1989</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1987, The Mineralogical Society</copyright-statement>
<copyright-year>1987</copyright-year>
<abstract>
<title>Abstract</title>
<p>Holtite, (Si<sub>2.25</sub>Sb<sub>0.75</sub>)B[Al<sub>6</sub>(Al<sub>0.43</sub>Ta<sub>0.27</sub>&#x25A1;<sub>0.30</sub>)O<sub>15</sub>(O,OH)<sub>2.25</sub>], is orthorhombic <italic>a</italic> = 4.6914(5), <italic>b</italic> = 11.896(2), c = 20.383(4)&#x00C5;, space group <italic>Pnma</italic>. Full-matrix least-squares refinement yielded a final <italic>R</italic> = 0.030, for 1664 reflections with <italic>I</italic> &#x2A7E; 3&#x03C3;(I). Its crystal structure is closely related to that of dumortierite, but with the difference that extensive substitution of Si by Sb occurs in holtite. SbO<sub>3</sub> triangular pyramids replace the SiO<sub>4</sub> tetrahedra arranged around the inside edge of the hexagonally shaped tunnels which are the feature of the dumortierite and holtite structures. Associated with these replacements is the replacement of Al by Ta in the octahedral site centred in these tunnels, and the development of vacancies in this metal site and its attached oxygens.</p></abstract>
<kwd-group>
<title>Keywords</title>
<kwd>holtite</kwd>
<kwd>crystal structure</kwd>
<kwd>crystal chemistry</kwd>
<kwd>Greenbushes</kwd>
<kwd>Australia</kwd>
</kwd-group>
</article-meta>
</front>
</article>
