<?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.1966.036.276.07</article-id>
<title-group>
<article-title>Heating Experiments on Gudmundite</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Horrell Clark</surname>
<given-names>A.</given-names>
</name>
<aff>Dept. of Geology, University College, London, W.C. 1</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>12</month>
<year>1966</year>
</pub-date>
<volume>36</volume>
<issue>276</issue>
<fpage>1123</fpage>
<lpage>1125</lpage>
<history>
<date date-type="received">
<day>6</day>
<month>6</month>
<year>1966</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1966, The Mineralogical Society</copyright-statement>
<copyright-year>1966</copyright-year>
<abstract>
<title>Summary</title>
<p>In the absence of published experimental data on phase equilibria in the ternary system Fe-Sb-S and on the stability relations of gudmundite (FeSbS) and berthierite (FeSb<sub>2</sub>S<sub>4</sub>) , some preliminary investigations on the upper stability limit of natural gudmundite are briefly described. On heating in vacuo, As-free gudmundite broke down between 269&#x00B0; and 288&#x00B0;C, an approximate upper stability limit of 280&#x00B1;10&#x00B0;C conforming to the stability relations of the associated phases.</p></abstract>
</article-meta>
</front>
</article>
