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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.1977.041.319.09</article-id>
<title-group>
<article-title>The Metavoltine Problem: Metavoltine from Madeni Zakh and Chuquicamata, and a Related Artificial Compound</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Scordari</surname>
<given-names>F.</given-names>
</name>
<aff>Istituto di Mineralogia dell'Universit&#x00E0; di Bari, Italy</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>9</month>
<year>1977</year>
</pub-date>
<volume>41</volume>
<issue>319</issue>
<fpage>371</fpage>
<lpage>374</lpage>
<history>
<date date-type="received">
<day>18</day>
<month>12</month>
<year>1975</year>
</date>
<date date-type="rev-recd">
<day>6</day>
<month>12</month>
<year>1976</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1977, The Mineralogical Society</copyright-statement>
<copyright-year>1977</copyright-year>
<abstract>
<title>Summary</title>
<p>Bandy (1938) described as metavoltine? a mineral coming from Chuquicamata (Chile) with chemical composition K<sub>2</sub>Na<sub>6</sub>Fe<sup>3+</sup>(SO<sub>4</sub>)<sub>12</sub>(OH)<sub>2</sub>&#x00B7;20H<sub>2</sub>O. Owing to some differences between this mineral and that first described by Blaas (1883), doubts persist on the identity of these two compounds. X-ray analyses were performed to clarify the relation between them. An artificial product, closely related to metavoltine as regards lattice and chemical composition, was also studied, and affords a better understanding of the Na and K diadochy already observed in metavoltine.</p></abstract>
</article-meta>
</front>
</article>
