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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.1987.051.360.10</article-id>
<title-group>
<article-title>New Data on the Relation Between Caryinite and Arseniopleite</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Dunn</surname>
<given-names>Pete J.</given-names>
</name>
<aff>Department of Mineral Sciences, Smithsonian Institution, Washington, D.C. 20560, USA</aff></contrib>
<contrib contrib-type="author">
<name>
<surname>Peacor</surname>
<given-names>Donald R.</given-names>
</name>
<aff>Department of Geological Sciences, University of Michigan, Ann Arbor, Michigan 48109, USA</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>6</month>
<year>1987</year>
</pub-date>
<volume>51</volume>
<issue>360</issue>
<fpage>281</fpage>
<lpage>284</lpage>
<history>
<date date-type="received">
<day>13</day>
<month>3</month>
<year>1986</year>
</date>
<date date-type="rev-recd">
<day>16</day>
<month>6</month>
<year>1986</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1987, The Mineralogical Society</copyright-statement>
<copyright-year>1987</copyright-year>
<abstract>
<title>Abstract</title>
<p>Caryinite from L&#x00E5;mgban, Sweden, and arseniopleite from both the L&#x00E5;ngban and Sj&#x00F6; Mines in Sweden, are re-examined chemically and crystallographically. Both species are monoclinic, with space group <italic>C2/c</italic>, and similar lattice parameters. The general formula for caryinite is Na<sub>4</sub>Ca<sub>4</sub>Ca<sub>4</sub>(Mn,Mg)<sub>8</sub>(AsO<sub>4</sub>)<sub>12</sub>, and that for arseniopleite is Na<sub>4</sub>Ca<sub>4</sub>Mn<sub>4</sub>(Mn,Mg)<sub>8</sub>(AsO<sub>4</sub>)<sub>12</sub>. The species status of arseniopleite remains uncertain; it may have Mn dominant in the <italic>M</italic>(1) site.</p></abstract>
<kwd-group>
<title>Keywords</title>
<kwd>caryinite</kwd>
<kwd>arseniopleite</kwd>
<kwd>arsenates</kwd>
<kwd>L&#x00E4;ngban</kwd>
<kwd>Sj&#x00F6; mines</kwd>
<kwd>Sweden</kwd>
</kwd-group>
</article-meta>
</front>
</article>
