<?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.1982.046.340.09</article-id>
<title-group>
<article-title>Dwornikite, (Ni,Fe)SO<sub>4</sub> &#x00B7; H<sub>2</sub>O, a Member of the Kieserite Group from Minasragra, Peru</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Milton</surname>
<given-names>Charles</given-names>
</name>
<aff>US Geological Survey and George Washington University</aff></contrib>
<contrib contrib-type="author">
<name>
<surname>Evans</surname>
<given-names>Howard T.</given-names><suffix>Jr.</suffix>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Johnson</surname>
<given-names>Robert G.</given-names>
</name></contrib>
<aff>US Geological Survey, National Center 959, Reston, Virginia 22092, USA</aff></contrib-group>
<pub-date pub-type="ppub">
<month>9</month>
<year>1982</year>
</pub-date>
<volume>46</volume>
<issue>340</issue>
<fpage>351</fpage>
<lpage>355</lpage>
<history>
<date date-type="received">
<day>28</day>
<month>9</month>
<year>1981</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1982, The Mineralogical Society</copyright-statement>
<copyright-year>1982</copyright-year>
<abstract>
<title>Abstract</title>
<p>Dwornikite, (Ni<sub>1&#x2212;<italic>x</italic></sub>Fe<sub><italic>x</italic></sub>)SO<sub>4</sub> &#x00B7; H<sub>2</sub>O is a member of the kieserite group, monoclinic with space group <italic>C</italic>2/<italic>c</italic>. Specimens from Minasragra, Peru with <italic>x</italic> &#x223C; 0.1 have a unit cell with <italic>a</italic> = 6.839(2), <italic>b</italic> = 7.582(2), <italic>c</italic> = 7.474(2) &#x00C5;, and <italic>&#x03B2;</italic> = 117.85(2)&#x00B0;. The six strongest lines of the powder pattern are: 3.342 (<inline-formula><mml:math><mml:mrow><mml:mover><mml:mn>1</mml:mn><mml:mo>&#x00AF;</mml:mo></mml:mover><mml:mn>12</mml:mn></mml:mrow></mml:math></inline-formula>, 100), 4.732 (110, 70), 3.024 (200, 70), 4.754 (<inline-formula><mml:math><mml:mrow><mml:mover><mml:mn>1</mml:mn><mml:mo>&#x00AF;</mml:mo></mml:mover><mml:mn>11</mml:mn></mml:mrow></mml:math></inline-formula>, 50), 3.293 (021, 35), 2.491 (022, 35). The mineral occurs as fine grained white aggregates associated with vanadium sulphide ores containing patronite and bravoite, mixed with other oxidation products. New unit cell data for the synthetic end-member compounds NiSO<sub>4</sub> &#x00B7; H<sub>2</sub>O and FeSO<sub>4</sub> &#x00B7; H<sub>2</sub>O, and new X-ray powder data for retgersite (NiSO<sub>4</sub> &#x00B7; 6H<sub>2</sub>O) are provided.</p></abstract>
</article-meta>
</front>
</article>
