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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.1960.032.250.06</article-id>
<title-group>
<article-title>A Thermal Study of Thaumasite</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Font-Altaba</surname>
<given-names>M.</given-names>
</name>
<aff>Instituto de Edafolog&#x00ED;a y Fisiolog&#x00ED;a Vegetal, Barcelona, Spain.</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>9</month>
<year>1960</year>
</pub-date>
<volume>32</volume>
<issue>250</issue>
<fpage>567</fpage>
<lpage>572</lpage>
<copyright-statement>Copyright &#x00A9; 1960, The Mineralogical Society</copyright-statement>
<copyright-year>1960</copyright-year>
<abstract>
<title>Summary</title>
<p>A differential thermal analysis curve of thaumasite shows an endothermal peak at 206&#x00B0; C., correspinding to the loss of H<sub>2</sub>O and CO<sub>2</sub>, and a weak exothermal peak at 709&#x00B0; C., corresponding to recrystallization to a mixture of anhydrite and larnite, as is shown by X-ray powder photographs of material heated to 950&#x00B0; C. Improved powder data for thaumasite are given: the three strongest lines are at 9&#x00B7;66, 3&#x00B7;79, and 4&#x00B7;58 &#x00C5;., and the cell-dimensions are <italic>a</italic> 10&#x00B7;992, <italic>c</italic> 10&#x00B7;311 &#x00C5;.</p></abstract>
</article-meta>
</front>
</article>
