<?xml version="1.0"?>
<!DOCTYPE article SYSTEM "journalpublishing.dtd">
<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.1969.037.288.05</article-id>
<title-group>
<article-title>Studies in the System BaO-Al<sub>2</sub>O<sub>3</sub>-SiO<sub>2</sub> III. The Binary System Sanbornite-celsian</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Lin</surname>
<given-names>H. C.</given-names>
</name>
<xref ref-type="author-notes" rid="FN1">1</xref></contrib>
<contrib contrib-type="author">
<name>
<surname>Foster</surname>
<given-names>W. R.</given-names>
</name></contrib>
<aff>Department of Mineralogy, The Ohio State University, Columbus, Ohio 43210, U.S.A.</aff></contrib-group>
<author-notes>
<fn fn-type="present-address" id="FN1"><label>1</label><p>Present address: Department of Geology Sciences, Queen's University, Kingston, Ontario, Canada.</p></fn></author-notes>
<pub-date pub-type="ppub">
<month>12</month>
<year>1969</year>
</pub-date>
<volume>37</volume>
<issue>288</issue>
<fpage>459</fpage>
<lpage>465</lpage>
<history>
<date date-type="received">
<day>24</day>
<month>2</month>
<year>1969</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1969, The Mineralogical Society</copyright-statement>
<copyright-year>1969</copyright-year>
<abstract>
<title>Summary</title>
<p>The system sanbornite-celsian has been investigated by the quenching method, and the results compared with earlier studies. The system is essentially a simple binary eutectic system with little or no solid solution. The eutectic is located at a composition of 69% sanbornite and 31% celsian (by weight) and at a temperature of 1227&#x00B1;3&#x00B0;C. No evidence for substantial solid solution of celsian in sanbornite, as reported in previous work, was found. Paracelsian, a naturally occurring polymorph of celsian, was not encountered in the study.</p></abstract>
</article-meta>
</front>
</article>
