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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.1995.059.395.13</article-id>
<article-categories>
<subj-group>
<subject>Mineralogy</subject>
</subj-group>
</article-categories>
<title-group>
<article-title>Hydrogen Bonding in Borcarite, an Unusual Borate-Carbonate Mineral</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Burns</surname>
<given-names>P. C.</given-names>
</name>
<xref ref-type="author-notes" rid="FN1">*</xref></contrib>
<contrib contrib-type="author">
<name>
<surname>Hawthorne</surname>
<given-names>F. C.</given-names>
</name></contrib>
<aff>Department of Geological Sciences, University of Manitoba, Winnipeg, Manitoba, Canada R3T 2N2</aff></contrib-group>
<author-notes>
<fn fn-type="present-address" id="FN1"><label>*</label><p>Present address: Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge CB2 3EQ, UK</p></fn></author-notes>
<pub-date pub-type="ppub">
<month>6</month>
<year>1995</year>
</pub-date>
<volume>59</volume>
<issue>395</issue>
<fpage>297</fpage>
<lpage>304</lpage>
<history>
<date date-type="received">
<day>1</day>
<month>6</month>
<year>1994</year>
</date>
<date date-type="rev-recd">
<day>17</day>
<month>8</month>
<year>1994</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1995, The Mineralogical Society</copyright-statement>
<copyright-year>1995</copyright-year>
<abstract>
<title>Abstract</title>
<p>The crystal structure, including hydrogen positions, of borcarite, Ca<sub>4</sub>Mg[B<sub>4</sub>O<sub>6</sub>(OH)<sub>6</sub>](CO<sub>3</sub>)<sub>2</sub>, monoclinic, <italic>a</italic> = 17.840(4), <italic>b</italic> = 8.380(2), <italic>c</italic> = 4.445(1) &#x00C5;, &#x03B2; = 102.04(3)&#x00B0;, <italic>V</italic> = 649.9(3) &#x00C5;<sup>3</sup>, space group <italic>C</italic>2/<italic>m</italic>, has been refined by full-matrix least-squares methods to <italic>R</italic> = 2.5% and <italic>wR</italic> = 3.0% for 1020 unique observed [&#x007C;<italic>F</italic>&#x007C; &#x2265; 5&#x03C3;(F)] reflections collected using Mo-<italic>K&#x03B1;</italic> X-radiation. The H positions were located on difference-Fourier maps and were refined using the &#x2018;soft&#x2019; constraint that O-H distances are &#x223C; 0.96 &#x00C5;. The 4:4T FBB (fundamental building block) of the borcarite structure contains four B&#x03C6;4 tetrahedra (&#x03C6; = unspecified ligand) which share corners to form a four-membered polyhedral ring. Borcarite is the only mineral known to contain this FBB. The FBBs do not polymerize, but each shares three anions with an Mg&#x03C6;<sub>6</sub> octahedron on either side, forming rods of composition [MgB<sub>4</sub>O<sub>6</sub>(OH)<sub>6</sub>]<sup>4-</sup> along the <italic>c</italic>-axis. The rigidity of these rods is enhanced by hydrogen bonding, and individual rods are connected through Ca&#x03C6;<sub>8</sub> polyhedra, C&#x03C6;<sub>3</sub> triangles and hydrogen bonds.</p></abstract>
<kwd-group>
<title>Keywords</title>
<kwd>borcarite</kwd>
<kwd>crystal structure</kwd>
<kwd>hydrogen bond</kwd>
<kwd>borate</kwd>
<kwd>Russia</kwd>
</kwd-group>
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