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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.1996.060.401.10</article-id>
<article-categories>
<subj-group subj-group-type="heading">
<subject>Mineralogy</subject>
</subj-group>
</article-categories>
<title-group>
<article-title>A Natural Ferrous Substituted Sal&#x00E9;ite from Arcu Su Linnarbu, Capoterra, Cagliari, Sardinia</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Vochten</surname>
<given-names>R.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Van Springel</surname>
<given-names>K.</given-names>
</name></contrib>
<aff>Laboratorium voor chemische en fysische mineralogie, Departement Scheikunde, Universiteit Antwerpen, Middelheimlaan 1, 2020 Antwerpen, Belgium</aff></contrib-group>
<pub-date pub-type="ppub">
<month>8</month>
<year>1996</year>
</pub-date>
<volume>60</volume>
<issue>401</issue>
<fpage>647</fpage>
<lpage>651</lpage>
<history>
<date date-type="received">
<day>9</day>
<month>5</month>
<year>1995</year>
</date>
<date date-type="rev-recd">
<day>24</day>
<month>7</month>
<year>1995</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1996, The Mineralogical Society</copyright-statement>
<copyright-year>1996</copyright-year>
<abstract>
<title>Abstract</title>
<p>Ferrous substituted sal&#x00E9;eite is a new variety of sal&#x00E9;eite from Arcu su Linnarbu, Sardinia. It is tetragonal with <italic>a</italic> = 6.982(2) <italic>c</italic> = 19.660(2) &#x00C5;, Z = 2; the ideal formula is (Mg,Fe<sup>2+</sup>)(UO<sub>2</sub>)<sub>2</sub>(PO<sub>4</sub>)<sub>2</sub>&#x00B7;4H<sub>2</sub>O. The strongest lines in the X-ray powder diffraction pattern are: 3.473(100)(114), 4.95(50)(110), 4.91(40)(004), 4.443(40)(112), 2.200(30)(118), 2.193(30)(303) and 2.178(30)(009). The mineral is light-yellow in colour and is dull fluorescent. The measured density is 3.242 g/cm<sup>3</sup> and Z = 2. There is a prominent (001) cleavage. Refractive indices are : &#x03B1; = 1.572(2) &#x03B2; = 1.577(2) &#x03B3; = 1.581(2) and 2V = 48&#x00B0;(2). The pleochroism is very weak and the elongation is positive parallel to Y. The mineral occurs as subparallel crystal aggregates with a quadratic outline.</p></abstract>
<kwd-group>
<title>Keywords</title>
<kwd>sal&#x00E9;eite</kwd>
<kwd>ferrous substitution</kwd>
<kwd>uranyl phosphate group</kwd>
<kwd>Arcu Su Linnarbu</kwd>
<kwd>Sardinia</kwd>
</kwd-group>
</article-meta>
</front>
</article>
