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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.1951.029.212.03</article-id>
<title-group>
<article-title>Priderite, a New Mineral from the Leucite-Lamproites of the West Kimberley Area, Western Australia</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Norrish</surname>
<given-names>K.</given-names>
</name><degrees>M.Sc.</degrees>
<aff>Research Officer of the Division of Soils, Commonwealth Scientific and Industrial Research Organization, Adelaide, South Australia.</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>3</month>
<year>1951</year>
</pub-date>
<volume>29</volume>
<issue>212</issue>
<fpage>496</fpage>
<lpage>501</lpage>
<copyright-statement>Copyright &#x00A9; 1951, The Mineralogical Society</copyright-statement>
<copyright-year>1951</copyright-year>
<abstract>
<title>Abstract</title>
<p>Priderite is the name suggested for a new mineral with the formula (K,Ba)<sub>1&#x00B7;3</sub>(Ti,Fe)<sub>8</sub>O<sub>16</sub>. X-ray diffraction studies show that the mineral is body-centred tetragonal with <italic>a</italic> 10&#x00B7;11, <italic>c</italic> 2&#x00B7;96 &#x00C5;. Structurally the mineral resembles cryptomelane, KMn<sub>8</sub>O<sub>16</sub>, the Ti of priderite being equivalent to the Mn of cryptomelane. Synthetic K- and Ba-priderites appear to be isostructural and they are probably members of a series analogous to cryptomelane-hollandite.</p></abstract>
</article-meta>
</front>
</article>
