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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.1993.057.386.15</article-id>
<article-categories>
<subj-group>
<subject>Crystal Structures</subject>
</subj-group>
</article-categories>
<title-group>
<article-title>Crystal Structure of KBSi<sub>3</sub>O<sub>8</sub> Isostructural with Danburite</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Kimata</surname>
<given-names>Mitsuyoshi</given-names>
</name>
<aff>Institute of Geoscience, University of Tsukuba, Ibaraki 305, Japan</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>3</month>
<year>1993</year>
</pub-date>
<volume>57</volume>
<issue>386</issue>
<fpage>157</fpage>
<lpage>164</lpage>
<history>
<date date-type="received">
<day>10</day>
<month>4</month>
<year>1990</year>
</date>
<date date-type="rev-recd">
<day>9</day>
<month>3</month>
<year>1992</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1993, The Mineralogical Society</copyright-statement>
<copyright-year>1993</copyright-year>
<abstract>
<title>Abstract</title>
<p>The crystal structure of KBSi<sub>3</sub>O<sub>8</sub> (orthorhombic, <italic>Pnam</italic>, with <italic>a</italic> = 8.683(1), <italic>b</italic> = 9.253(1), <italic>c</italic> = 8.272(1) &#x00C5;, V = 664.4(1) &#x00C5;<sup>3</sup>, <italic>Z</italic> = 4) has been determined by the direct method applied to 3-dimensional reflection data. The structure of a microcrystal with the dimensions 20 &#x00D7; 29 &#x00D7; 37 &#x00B5;m was refined to an unweighted residual of <italic>R</italic> = 0.031 using 386 non-zero structure amplitudes. KBSi<sub>3</sub>O<sub>8</sub> adopts a structure essentially different from reedmergneritc NaBSi<sub>3</sub>O<sub>8</sub>, with the low albite (NaAlSi<sub>3</sub>O<sub>8</sub>) structure, and isotypic with danburite CaB<sub>2</sub>Si<sub>2</sub>O<sub>8</sub> which has the same topology as paracelsian BaAl<sub>2</sub>Si<sub>2</sub>O<sub>8</sub>. The chemical relationship between this sample and danburite gives insight into a new coupled substitution; K<sup>+</sup> + Si<sup>4+</sup> = Ca<sup>2+</sup> + B<sup>3+</sup> in the extraframework and tetrahedral sites. The present occupancy refinement revealed partial disordering of B and Si atoms which jointly reside in two kinds of general equivalent points, <italic>T</italic>(1) and <italic>T</italic>(2) sites. Thus the expanded crystal-chemical formula can be written in the form K(B<sub>0.44</sub>Si<sub>0.56</sub>)<sub>2</sub>(B<sub>0.06</sub>Si<sub>0.94</sub>)<sub>2</sub>O<sub>8</sub>.</p>
<p>The systematic trend among crystalline compounds with the <italic>M</italic><sup>+</sup><italic>T</italic><sup>3+</sup><italic>T</italic><sup>4+</sup><sub>3</sub>O<sub>8</sub> formula suggests that they exist in one of four structural types; the feldspar structures with <italic>T</italic><sup>3+</sup>/<italic>T</italic><sup>4+</sup> ordered and/or disordered forms, and the paracelsian and the hollandite structures.</p></abstract>
<kwd-group>
<title>Keywords</title>
<kwd>danburite</kwd>
<kwd>crystal structure</kwd>
<kwd>feldspar</kwd>
<kwd>paracelsian</kwd>
<kwd>hollandite</kwd>
<kwd>reedmergnerite</kwd>
</kwd-group>
</article-meta>
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