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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.1983.047.343.12</article-id>
<title-group>
<article-title>New Data on Georgiadesite</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Rouse</surname>
<given-names>Roland C.</given-names>
</name>
<aff>Department of Geological Sciences, University of Michigan, Ann Arbor, Michigan 48109, USA</aff></contrib>
<contrib contrib-type="author">
<name>
<surname>Dunn</surname>
<given-names>Pete J.</given-names>
</name>
<aff>Department of Mineral Sciences, Smithsonian Institution, Washington, DC 20560, USA</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>6</month>
<year>1983</year>
</pub-date>
<volume>47</volume>
<issue>343</issue>
<fpage>219</fpage>
<lpage>220</lpage>
<history>
<date date-type="received">
<day>21</day>
<month>6</month>
<year>1982</year>
</date>
<date date-type="rev-recd">
<day>1</day>
<month>10</month>
<year>1982</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1983, The Mineralogical Society</copyright-statement>
<copyright-year>1983</copyright-year>
<abstract>
<title>Abstract</title>
<p>The chemistry and crystallography of type georgiadesite from Laurion, Greece, have been reexamined using electron microprobe analysis along with powder and single-crystal X-ray diffraction. Georgiadesite is monoclinic, <italic>P</italic>2<sub>1</sub>/<italic>c</italic>, with <italic>a</italic> = 13.803(10), <italic>b</italic> = 7.910(2), <italic>c</italic> = 10.812(4) &#x00C5;, and <italic>&#x03B2;</italic> = 102.68(3)&#x00B0;. No twinning was observed. The probable chemical formula is either Pb<sub>16</sub>(AsO<sub>4</sub>)<sub>4</sub>Cl<sub>14</sub>O<sub>2</sub>(OH)<sub>2</sub> or Pb<sub>16</sub>(AsO<sub>4</sub>)<sub>4</sub>Cl<sub>14</sub>(OH)<sub>6</sub>. The calculated densities for these formulae are 6.39 and 6.44 g/cm<sup>3</sup>, respectively, compared to a measured value of 6.3 + 0.3 g/cm<sup>3</sup>.</p></abstract>
</article-meta>
</front>
</article>
