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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.1992.056.382.08</article-id>
<article-categories>
<subj-group>
<subject>Mineralogy and Petrology</subject>
</subj-group>
</article-categories>
<title-group>
<article-title>Tooeleite, A New Mineral from the U.S. Mine, Tooele County, Utah</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Cesbron</surname>
<given-names>Fabien P.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Williams</surname>
<given-names>Sidney A.</given-names>
</name></contrib>
<aff>Globo De Plomo Enterprises, P.O. Box 872, Douglas AZ 85608, U.S.A.</aff></contrib-group>
<pub-date pub-type="ppub">
<month>3</month>
<year>1992</year>
</pub-date>
<volume>56</volume>
<issue>382</issue>
<fpage>71</fpage>
<lpage>73</lpage>
<copyright-statement>Copyright &#x00A9; 1992, The Mineralogical Society</copyright-statement>
<copyright-year>1992</copyright-year>
<abstract>
<title>Abstract</title>
<p>The new mineral tooeleite occurs with pyrite, arsenopyrite, scorodite, and jarosite at the U.S. Mine, Tooele Country, Utah. Analysis by electron microprobe gave Fe<sub>2</sub>O<sub>3</sub> 43.56%, As<sub>2</sub>O<sub>5</sub> 38.61%, SO<sub>3</sub> 7.24%, and H<sub>2</sub>O by the Penfield method 9.80%. For this analysis, the suggested formula is <inline-formula><mml:math><mml:mrow><mml:msubsup><mml:mrow><mml:mi>Fe</mml:mi></mml:mrow><mml:mrow><mml:mn>8</mml:mn><mml:mo>&#x2212;</mml:mo><mml:mn>2</mml:mn><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:mrow><mml:mo>[</mml:mo><mml:mrow><mml:mo>(</mml:mo><mml:msub><mml:mi>AS</mml:mi><mml:mrow><mml:mn>1</mml:mn><mml:mo>&#x2212;</mml:mo><mml:mi>x</mml:mi></mml:mrow></mml:msub><mml:msub><mml:mi>S</mml:mi><mml:mi>x</mml:mi></mml:msub><mml:mo>)</mml:mo></mml:mrow><mml:msub><mml:mo>O</mml:mo><mml:mn>4</mml:mn></mml:msub><mml:mo>]</mml:mo></mml:mrow><mml:mn>6</mml:mn></mml:msub><mml:msub><mml:mrow><mml:mo>(</mml:mo><mml:mi>OH</mml:mi><mml:mo>)</mml:mo></mml:mrow><mml:mn>6</mml:mn></mml:msub><mml:mo>.</mml:mo><mml:mn>5</mml:mn><mml:msub><mml:mo>H</mml:mo><mml:mn>2</mml:mn></mml:msub><mml:mo>O</mml:mo></mml:mrow></mml:math></inline-formula>; <italic>x</italic> is about 0.2.</p>
<p>Crystals are orthorhombic, perhaps <italic>Pbcm</italic> or <italic>Pbc</italic>2<sub>1</sub>, with <italic>a</italic> = 6.416, <italic>b</italic> 19.45, <italic>c</italic> = 8.941 &#x00C5;. The strongest diffraction lines are [<italic>d</italic> in &#x00C5;, (hkl), (I)] 9.75 (020) (10); 3.208 (200,132) (9); 3.047 (061,220) (5); 4.476 (&#x007B;002) (4) and 2.680 (240,113) (4). The mineral is optically negative with a small 2V; &#x03B1; = 1.94, &#x03B2; = 2.05, &#x03B3; = 2.06. Hardness = 3, D<sub>meas</sub> = 4.23, D<sub>calc</sub> = 4.15 g/cm<sup>3</sup> for Z = 2.</p></abstract>
<kwd-group>
<title>Keywords</title>
<kwd>tooeleite</kwd>
<kwd>new mineral</kwd>
<kwd>Tooele County</kwd>
<kwd>Utah</kwd>
</kwd-group>
</article-meta>
</front>
</article>
