<?xml version="1.0"?>
<!DOCTYPE article SYSTEM "journalpublishing.dtd">
<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.1967.036.277.01</article-id>
<title-group>
<article-title>Anandite, a New Barium Iron Silicate from Wilagedera, North Western Province, Ceylon</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Pattiaratchi</surname>
<given-names>D. B.</given-names>
</name>
<aff>Geological Survey Department, Ceylon</aff></contrib>
<contrib contrib-type="author">
<name>
<surname>Saari</surname>
<given-names>Esko</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Sahama</surname>
<given-names>Th. G.</given-names>
</name></contrib>
<aff>University of Helsinki, Finland</aff></contrib-group>
<pub-date pub-type="ppub">
<month>3</month>
<year>1967</year>
</pub-date>
<volume>36</volume>
<issue>277</issue>
<fpage>1</fpage>
<lpage>4</lpage>
<history>
<date date-type="received">
<day>10</day>
<month>8</month>
<year>1966</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1967, The Mineralogical Society</copyright-statement>
<copyright-year>1967</copyright-year>
<abstract>
<title>Summary</title>
<p>Anandite is a new barium iron silicate found in the magnetite ore zone of the Wilagedera iron ore body, in the North Western Province of Ceylon. The mineral is named after the late Dr. Ananda Coomaraswamy, the first director of the Mineral Survey of Ceylon.</p>
<p>Anandite is monoclinic, with <italic>a</italic> 5&#x00B7;412, <italic>b</italic> 9&#x00B7;434, <italic>c</italic> 19&#x00B7;953 &#x00C5;, <italic>&#x03B2;</italic> 94&#x00B0; 52&#x2032;, space group <italic>C</italic>2/<italic>c. D</italic> 3&#x00B7;94, hardness 3&#x2013;4. Optically positive, <italic>b</italic> &#x2016; <italic>&#x03B2;</italic>, <italic>&#x03B3;</italic> &#x2227; <italic>a</italic> 12&#x00B0;, <italic>&#x03B2;</italic> 1&#x00B7;85<sub>5</sub>, <italic>&#x03B3;</italic> &#x003E; 1&#x00B7;88. Pleochroism: <italic>&#x03B2;</italic> green, <italic>&#x03B3;</italic> brown. Chemical composition corresponds to the simplified formula (Ba,K) (Fe,Mg)<sub>a</sub> (Si,Al,Fe)<sub>4</sub>O<sub>10</sub> (O,OH)<sub>2</sub> with <italic>Z</italic> = 2. The data available indicate that the mineral has the trioctahedral structure of the brittle micas.</p></abstract>
</article-meta>
</front>
</article>
