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<article article-type="research-article">
<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.1989.053.369.09</article-id>
<article-categories>
<subj-group subj-group-type="heading">
<subject>Mineralogy</subject>
</subj-group>
</article-categories>
<title-group>
<article-title>A Barian Bannisterite from Japan</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Matsubara</surname>
<given-names>S.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Kato</surname>
<given-names>A.</given-names>
</name></contrib>
<aff>Department of Geology, National Science Museum, 3-23-1 Hyakunin-cho, Shinjuku, Tokyo 169, Japan</aff></contrib-group>
<pub-date pub-type="ppub">
<month>3</month>
<year>1989</year>
</pub-date>
<volume>53</volume>
<issue>369</issue>
<fpage>85</fpage>
<lpage>87</lpage>
<copyright-statement>Copyright &#x00A9; 1989, The Mineralogical Society</copyright-statement>
<copyright-year>1989</copyright-year>
<abstract>
<title>Abstract</title>
<p>Chemical analyses of bannisterite from the Kamo mine, Toba City, Mie Prefecture, Japan, give Ba : Ca = 69:31&#x2013;55:45, yielding the ideal formula with Ba &#x003E; Ca, i.e. (Ba,Ca)(K,H<sub>3</sub>O)(Mn<sup>2+</sup> &#x00B7; Mg,Fe<sup>2+</sup>)<sub>21</sub> (Si,Al)<sub>32</sub>(O,OH)<sub>92</sub> &#x00B7; <italic>n</italic>H<sub>2</sub>O, where Ba &#x003E; Ca, Mn<sup>2+</sup> &#x003E; Mg, Fe<sup>2+</sup>,Si &#x226B; Al, and O &#x003E; OH. The unit cell parameters calculated after the indexing of the X-ray powder pattern are: <italic>a</italic> = 22.95, <italic>b</italic> = 16.52, <italic>c</italic> = 25.66 &#x00C5;, <italic>&#x03B2;</italic> = 94.2&#x00B0;. It occurs as dark brown veinlets cutting massive caryopilite-rhodochrosite ore, which is also cut by veinlets of manganoan chlorite (Mn/(Mg + Mn + Fe) = <italic>c.</italic> 0.30&#x2013;0.39) with minor barian orthoclase (Ba/(K+ Ba) = 0.05 &#x223C; 0.06).</p></abstract>
<kwd-group>
<title>Keywords</title>
<kwd>barium</kwd>
<kwd>bannisterite</kwd>
<kwd>Japan</kwd>
<kwd>Kamo mine</kwd>
</kwd-group>
</article-meta>
</front>
</article>
