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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.1977.041.320.07</article-id>
<title-group>
<article-title>An Intergrowth of Calcic Labradorite in a Plagioclase-Quartz-Biotite Gneiss from Broken Hill, New South Wales</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Phillips</surname>
<given-names>Evan R.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Chenhall</surname>
<given-names>Bryan E.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Stone</surname>
<given-names>Ian J.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Pemberton</surname>
<given-names>J. W.</given-names>
</name></contrib>
<aff>Department of Geology, University of Wollongong, Wollongong, N.S.W. 2500, Australia</aff></contrib-group>
<pub-date pub-type="ppub">
<month>12</month>
<year>1977</year>
</pub-date>
<volume>41</volume>
<issue>320</issue>
<fpage>469</fpage>
<lpage>471</lpage>
<history>
<date date-type="received">
<day>29</day>
<month>11</month>
<year>1976</year>
</date>
<date date-type="rev-recd">
<day>4</day>
<month>1</month>
<year>1977</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1977, The Mineralogical Society</copyright-statement>
<copyright-year>1977</copyright-year>
<abstract>
<title>Summary</title>
<p>Compositions of An<sub>61</sub> and An<sub>69&#x00B7;5</sub> have been determined for two domains in plagioclase from a gneiss. Optical properties indicate that the same compositions apply respectively for an intergrowth of &#x2018;matrix&#x2019; and lamellae found in zones between the domains. The intergrowth appears to span the composition range between the B&#x00F8;ggild and Huttenlocher intergrowths.</p></abstract>
</article-meta>
</front>
</article>
