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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.1979.043.325.03</article-id>
<title-group>
<article-title>Kleemanite, a New Zinc Aluminium Phosphate</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Pilkington</surname>
<given-names>E. S.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Segnit</surname>
<given-names>E. R.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Watts</surname>
<given-names>J.</given-names>
</name></contrib>
<aff>CSIRO Division of Mineral Chemistry, Port Melbourne, Australia</aff></contrib-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Francis</surname>
<given-names>G.</given-names>
</name>
<aff>Iron Knob, South Australia</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>3</month>
<year>1979</year>
</pub-date>
<volume>43</volume>
<issue>325</issue>
<fpage>93</fpage>
<lpage>95</lpage>
<history>
<date date-type="received">
<day>10</day>
<month>8</month>
<year>1978</year>
</date>
<date date-type="rev-recd">
<day>23</day>
<month>10</month>
<year>1978</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1979, The Mineralogical Society</copyright-statement>
<copyright-year>1979</copyright-year>
<abstract>
<title>Summary</title>
<p>A new hydrated zinc aluminium phosphate mineral has the composition ZnAl<sub>2</sub>(PO<sub>4</sub>)<sub>2</sub>(OH)<sub>2</sub>.3H<sub>2</sub>O. It has been named kleemanite. It occurred rarely both as veinlets 1&#x2013;2 mm thick, and as thin layers on surfaces of cracks and small cavities in one section of the iron ore deposit at Iron Knob, South Australia. Chemical, X-ray, thermal analysis, and optical data are given.</p></abstract>
</article-meta>
</front>
</article>
