<?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.1993.057.389.10</article-id>
<title-group>
<article-title>Brianyoungite, a New Mineral Related to Hydrozincite, from the North of England Orefield</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Livingstone</surname>
<given-names>A.</given-names>
</name>
<aff>Department of Geology, Royal Museum of Scotland, Chambers Street, Edinburgh EH1 1JF</aff></contrib>
<contrib contrib-type="author">
<name>
<surname>Champness</surname>
<given-names>P. E.</given-names>
</name>
<aff>Department of Geology, The University of Manchester, Oxford Road, Manchester M13 9PL</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>12</month>
<year>1993</year>
</pub-date>
<volume>57</volume>
<issue>389</issue>
<fpage>665</fpage>
<lpage>670</lpage>
<history>
<date date-type="received">
<day>12</day>
<month>11</month>
<year>1992</year>
</date>
<date date-type="rev-recd">
<day>12</day>
<month>3</month>
<year>1993</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1993, The Mineralogical Society</copyright-statement>
<copyright-year>1993</copyright-year>
<abstract>
<title>Abstract</title>
<p>Brianyoungite, which is chemically and structurally related to hydrozincite, occurs as white rosettes (&#x003C;100 &#x00B5;m) with gypsum on rubbly limestone within the oxidised zone at Brownley Hill Mine, Nenthead, Cumbria. The mineral contains (wt.%) 71.47 ZnO, 9.90 CO<sub>2</sub>, 6.62 SO<sub>3</sub> and 10.70 H<sub>2</sub>O<sup>+</sup>. Based on 29 oxygen atoms, the empirical formula is Zn<sub>11.73</sub>[(CO<sub>3</sub>)<sub>3.00</sub>,(SO<sub>4</sub>)<sub>1.10</sub>]<sub>4.10</sub>(OH)<sub>15.88</sub> or ideally Zn<sub>3</sub>(CO<sub>3</sub>,SO<sub>4</sub>)(OH)<sub>4</sub>. Brianyoungite is either orthorhombic or monoclinic with &#x03B2; very close to 90&#x00B0;. Cell parameters determined by electron diffraction and refined from X-ray powder diffraction data are <italic>a</italic> = 15.724, <italic>b</italic> = 6.256 and <italic>c</italic> = 5.427 &#x00C5;. Density is &#x003E; 3.93, &#x003C; 4.09 g/cm<sup>3</sup> (meas.) and 4.11 g/cm<sup>3</sup> (calc.); Z = 4. Thermogravimetric analysis, IR and XRD powder data (23 lines) are presented.</p></abstract>
<kwd-group>
<title>Keywords</title>
<kwd>brianyoungite</kwd>
<kwd>hydrozincite</kwd>
<kwd>Cumbria</kwd>
<kwd>new mineral</kwd>
</kwd-group>
</article-meta>
</front>
</article>
