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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.1971.038.295.05</article-id>
<title-group>
<article-title>The Stability and Natural Occurrence of Margarite</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Velde</surname>
<given-names>Bruce</given-names>
</name>
<aff>Laboratoire de P&#x00E9;trographie, Facult&#x00E9; des Sciences de Paris, 9 quai Saint Bernard, Paris 5</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>9</month>
<year>1971</year>
</pub-date>
<volume>38</volume>
<issue>295</issue>
<fpage>317</fpage>
<lpage>323</lpage>
<history>
<date date-type="received">
<day>1</day>
<month>5</month>
<year>1970</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1971, The Mineralogical Society</copyright-statement>
<copyright-year>1971</copyright-year>
<abstract>
<title>Summary</title>
<p>The upper stability of margarite has been determined to be 450 &#x00B0;C at 1 kb and 530 &#x00B0;C at 2 kb total pressure (P<sub>H<sub>2</sub>O</sub> = P<sub>total</sub>). Other experiments delimit in a general way the lower stability of this mineral and its paragenesis in more SiO<sub>2</sub> rich compositions. The presence of the 060 reflection at 1&#x00B7;475 &#x00C5; can be used to distinguish between margarite and paragonite or muscovite.</p></abstract>
</article-meta>
</front>
</article>
