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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.1994.058.393.07</article-id>
<article-categories>
<subj-group subj-group-type="heading">
<subject>Mineralogy</subject>
</subj-group>
</article-categories>
<title-group>
<article-title>Mineralogical Nomenclature: Pseudorutile Revalidated and Neotype Given</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Grey</surname>
<given-names>Ian E.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Watts</surname>
<given-names>John A.</given-names>
</name></contrib>
<aff>CSIRO Mineral Products, P.O. Box 124, Port Melbourne, Vic 3207, Australia</aff></contrib-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Bayliss</surname>
<given-names>Peter</given-names>
</name>
<aff>Australian Museum, P.O. Box A285, Sydney, N.S.W. 2000, Australia</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>12</month>
<year>1994</year>
</pub-date>
<volume>58</volume>
<issue>393</issue>
<fpage>597</fpage>
<lpage>600</lpage>
<history>
<date date-type="received">
<day>30</day>
<month>11</month>
<year>1993</year>
</date>
<date date-type="rev-recd">
<day>25</day>
<month>3</month>
<year>1994</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1994, The Mineralogical Society</copyright-statement>
<copyright-year>1994</copyright-year>
<abstract>
<title>Abstract</title>
<p>Pseudorutile, <inline-formula><mml:math><mml:mrow><mml:msubsup><mml:mrow><mml:mi>Fe</mml:mi></mml:mrow><mml:mrow><mml:mn>2</mml:mn></mml:mrow><mml:mrow><mml:mn>3</mml:mn><mml:mo>&#x002B;</mml:mo></mml:mrow></mml:msubsup><mml:msub><mml:mi>Ti</mml:mi><mml:mn>3</mml:mn></mml:msub><mml:msub><mml:mi>O</mml:mi><mml:mn>9</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>, has recently been revalidated as a mineral species, and the neotype locality is now South Neptune Island, South Australia. Powder X-ray diffraction data are given on a hexagonal primitive unit cell with <italic>a</italic> = 2.8667(5) and <italic>c</italic> = 4.5985(9) &#x00C5;. Leucoxene, arizonite and proarizonite are considered to be mixtures. Kleberite is considered to be a hydroxylian pseudorutile, <inline-formula><mml:math><mml:mrow><mml:msubsup><mml:mrow><mml:mi>Fe</mml:mi></mml:mrow><mml:mrow><mml:mn>2</mml:mn><mml:mo>&#x2212;</mml:mo><mml:mi>x</mml:mi></mml:mrow><mml:mrow><mml:mn>3</mml:mn><mml:mo>&#x002B;</mml:mo></mml:mrow></mml:msubsup><mml:msub><mml:mi>Ti</mml:mi><mml:mn>3</mml:mn></mml:msub><mml:msub><mml:mi>O</mml:mi><mml:mrow><mml:mn>9</mml:mn><mml:mo>&#x2212;</mml:mo><mml:mn>3</mml:mn><mml:mi>x</mml:mi></mml:mrow></mml:msub><mml:msub><mml:mo>(</mml:mo><mml:mi>OH</mml:mi><mml:mo>)</mml:mo><mml:mrow><mml:mn>3</mml:mn><mml:mi>x</mml:mi></mml:mrow></mml:msub></mml:mrow></mml:math></inline-formula>.</p></abstract>
<kwd-group>
<title>Keywords</title>
<kwd>pseudorutile</kwd>
<kwd>arizonite</kwd>
<kwd>proarizonite</kwd>
<kwd>leucoxene</kwd>
<kwd>kleberite</kwd>
<kwd>type specimen</kwd>
<kwd>type locality</kwd>
</kwd-group>
</article-meta>
</front>
</article>
