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<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.1974.039.305.11</article-id>
<title-group>
<article-title>Magnesian Collinsite from Milgun Station, Western Australia</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Bridge</surname>
<given-names>P. J.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Pryce</surname>
<given-names>M. W.</given-names>
</name></contrib>
<aff>Government Chemical Laboratories, Perth, Western Australia</aff></contrib-group>
<pub-date pub-type="ppub">
<month>3</month>
<year>1974</year>
</pub-date>
<volume>39</volume>
<issue>305</issue>
<fpage>577</fpage>
<lpage>579</lpage>
<history>
<date date-type="received">
<day>4</day>
<month>6</month>
<year>1973</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1974, The Mineralogical Society</copyright-statement>
<copyright-year>1974</copyright-year>
<abstract>
<title>Summary</title>
<p>An occurrence of magnesian collinsite has been found with other rare phosphates in a variscite deposit in semi-desert 15 km NW. of Milgun Station homestead (25&#x00B0; 6&#x2032; S., 118&#x00B0; 18&#x2032; E.), Western Australia. The collinsite occurs as tapering white 3-mm prisms, mammillated aggregates, and thin veinlets in cavities in mudstone. The crystals have two good cleavages, D2.93, subvitreous lustre, H4&#x2013;5, white streak and are brittle. Optical properties <italic>&#x03B1;</italic> 1&#x00B7;632, <italic>&#x03B2;</italic> 1&#x00B7;642, <italic>&#x03B3;</italic> 1&#x00B7;657, 2V<italic>&#x03B3;</italic> , &#x2248; 80&#x00B0;. The mineral is triclinic with <italic>a</italic> 5&#x00B7;734, <italic>b</italic> 6&#x00B7;780, <italic>c</italic> 5&#x00B7;441 &#x00C5;, &#x03B1;97&#x00B7;29&#x00B0; <italic>&#x03B2;</italic> 108&#x00B7;56&#x00B0;, <italic>&#x03B3;</italic> 107&#x00B7;28&#x00B0;. X-ray powder data given, the lines are similar to P.D.F. card 14&#x2013;314 but new cell gives better indexing. Chemical analysis by F. R. W. Lindsey gave FeO 0&#x00B7;07, MgO 11&#x00B7;3, CaO 35&#x00B7;2, Na<sub>2</sub>O 0&#x00B7;01, K<sub>2</sub>O 0&#x00B7;02, P<sub>2</sub>O<sub>5</sub> 41&#x00B7;2, H<sub>2</sub>O<sup>+</sup>10&#x00B7;7, H<sub>2</sub>O<sup>&#x2212;</sup> 0&#x00B7;15, F 0&#x00B7;02, SiO<sub>2</sub> (quartz impurity) 1&#x00B7;31, Al, Mn, Zn, SO<sub>3</sub> not detected, net sum 99&#x00B7;97, close to Ca<sub>2</sub>Mg(PO<sub>4</sub>)<sub>2</sub>.2H<sub>2</sub>O, after deduction of moisture and quartz impurity. Typical specimens are preserved at the Government Chemical Laboratories, Perth, Western Australia.</p></abstract>
</article-meta>
</front>
</article>
