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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.1956.031.234.06</article-id>
<title-group>
<article-title>The section CaSiO<sub>3</sub>-MgSiO<sub>3</sub>-Al<sub>2</sub>O<sub>3</sub></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Segnit</surname>
<given-names>E. R.</given-names>
</name> <degrees>M.Sc., Ph.D.</degrees>
<aff>Department of Geology, University of Adelaide<sup>1</sup></aff></contrib></contrib-group>
<author-notes>
<fn fn-type="other" id="FN"><label>1</label><p>The greater part of this work was done whilst the author was a research student in the Dept. of Mineralogy and Petrology, University of Cambirdge.</p></fn></author-notes>
<pub-date pub-type="ppub">
<month>9</month>
<year>1956</year>
</pub-date>
<volume>31</volume>
<issue>234</issue>
<fpage>255</fpage>
<lpage>264</lpage>
<copyright-statement>Copyright &#x00A9; 1956, The Mineralogical Society</copyright-statement>
<copyright-year>1956</copyright-year>
<abstract>
<title>Summary</title>
<p>Phase relationships in the section CaSiO<sub>3</sub>-MgSiO<sub>3</sub>-Al<sub>2</sub>O<sub>3</sub> through the quaternary system CaO-MgO-Al<sub>2</sub>O<sub>3</sub>-SiO<sub>2</sub> have been determined. The bearing of the results on the genesis of aluminous pyroxenes and associated minerals in metamorphic rocks is discussed.</p></abstract>
</article-meta>
</front>
</article>
