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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.1977.041.319.11</article-id>
<title-group>
<article-title>On the Occurrence of Smolyaninovite in the Mount Cobalt Deposit, in North-Western Queensland, Australia</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Smith</surname>
<given-names>L. K.</given-names>
</name>
<xref ref-type="author-notes" rid="FN1">1</xref></contrib>
<contrib contrib-type="author">
<name>
<surname>Han</surname>
<given-names>K. N.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Lawson</surname>
<given-names>F.</given-names>
</name></contrib>
<aff>Department of Chemical Engineering, Monash University, Clayton, Victoria, 3168, Australia</aff></contrib-group>
<author-notes>
<fn fn-type="present-address" id="FN1"><label>1</label><p>Present address: I.C.I. Central Research Laboratories, Ascot Vale, Victoria, 3032, Australia.</p></fn></author-notes>
<pub-date pub-type="ppub">
<month>9</month>
<year>1977</year>
</pub-date>
<volume>41</volume>
<issue>319</issue>
<fpage>385</fpage>
<lpage>388</lpage>
<history>
<date date-type="received">
<day>15</day>
<month>4</month>
<year>1975</year>
</date>
<date date-type="rev-recd">
<day>13</day>
<month>3</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>Smolyaninovite, (Co, Ni, Ca, Mg)<sub>3</sub> (Fe, Al)<sub>2</sub> (AsO<sub>4</sub>)<sub>4</sub>. 11H<sub>2</sub>O, has recently been recognized in the mineralized region around Mount Cobalt, Queensland. It is a soft polycrystalline earthy yellow-brown material, is probably the weathering product of cobaltian arsenopyrite or alloclase, and shows para-magnetic properties.</p></abstract>
</article-meta>
</front>
</article>
