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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.1972.038.299.02</article-id>
<title-group>
<article-title>Embreyite, a New Mineral from Berezov, Siberia</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Williams</surname>
<given-names>S. A.</given-names>
</name>
<xref ref-type="author-notes" rid="FN1">1</xref>
<aff>British Museum (Natural History), Cromwell Road, London S.W. 7</aff></contrib></contrib-group>
<author-notes>
<fn fn-type="present-address" id="FN1"><label>1</label><p>Permanent address: Phelps Dodge Corpn., Douglas, Arizona 856o7.</p></fn></author-notes>
<pub-date pub-type="ppub">
<month>9</month>
<year>1972</year>
</pub-date>
<volume>38</volume>
<issue>299</issue>
<fpage>790</fpage>
<lpage>793</lpage>
<history>
<date date-type="received">
<day>18</day>
<month>10</month>
<year>1971</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1972, The Mineralogical Society</copyright-statement>
<copyright-year>1972</copyright-year>
<abstract>
<title>Summary</title>
<p>Embreyite is a new mineral that has been found only in old specimens collected at Berezov, Siberia. The composition is Pb<sub>4&#x00B7;97</sub>(CrO<sub>4</sub>)<sub>2&#x00B7;00</sub>(PO<sub>4</sub>)<sub>1&#x00B7;91</sub>.0&#x00B7;75H<sub>2</sub>O, or Pb<sub>5</sub>(CrO<sub>4</sub>)<sub>2</sub>(PO<sub>4</sub>)<sub>2</sub>. H<sub>2</sub>O based on both wet and electron-probe analyses. Z = I, <italic>D</italic><sub>meas</sub> 6&#x00B7;45, <italic>D</italic><sub>eale</sub> 6&#x00B7;41. Crystals are monoclinic with <italic>a</italic> 9&#x00B7;755 &#x00C5;, <italic>b</italic> 5&#x00B7;636, <italic>c</italic> 7&#x00B7;135, <italic>&#x03B2;</italic> 103&#x00B0;5&#x2032; the space group may be <italic>P</italic>2<sub>1</sub>/<italic>m</italic>. No single crystals were found. <italic>&#x03B1;</italic> = 2&#x00B7;20, <italic>&#x03B2;</italic> = <italic>&#x03B3;</italic> = 2&#x00B7;36. Colour in various shades of orange with a yellow streak. H = 3&#x00BD;; no cleavages observed. Occurs with vauquelinite, crocoite, and phoenicochroite in the oxide zone assemblage from Berezov.</p></abstract>
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