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<article article-type="research-article">
<front>
<journal-meta>
<journal-id journal-id-type="archive">gsminmag</journal-id>
<journal-title>Clay Minerals</journal-title>
<abbrev-journal-title abbrev-type="full">Clay Minerals</abbrev-journal-title>
<issn pub-type="ppub">0009-8558</issn>
<publisher>
<publisher-name>Mineralogical Society</publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.1180/minmag.1975.040.310.01</article-id>
<title-group>
<article-title>Tacharanite</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Cliff</surname>
<given-names>G.</given-names>
</name>
<xref ref-type="aff" rid="A1">1</xref></contrib>
<contrib contrib-type="author">
<name>
<surname>Gard</surname>
<given-names>J. A.</given-names>
</name>
<xref ref-type="aff" rid="A2">2</xref></contrib>
<contrib contrib-type="author">
<name>
<surname>Lorimer</surname>
<given-names>G. W.</given-names>
</name>
<xref ref-type="aff" rid="A1">1</xref></contrib>
<contrib contrib-type="author">
<name>
<surname>Taylor</surname>
<given-names>H. F. W.</given-names>
</name>
<xref ref-type="aff" rid="A2">2</xref></contrib></contrib-group>
<aff id="A1"><label>1</label>Department of Metallurgy, The University, Manchester, England</aff>
<aff id="A2"><label>2</label>Department of Chemistry, University of Aberdeen, Scotland</aff>
<pub-date pub-type="ppub">
<month>6</month>
<year>1975</year>
</pub-date>
<volume>40</volume>
<issue>310</issue>
<fpage>113</fpage>
<lpage>126</lpage>
<history>
<date date-type="received">
<day>17</day>
<month>6</month>
<year>1974</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1975, The Mineralogical Society</copyright-statement>
<copyright-year>1975</copyright-year>
<abstract>
<title>Summary</title>
<p>Tacharanite has been re-examined using electron microscopy and diffraction, analytical microscopy, X-ray powder and fibre rotation photographs, and other methods. The composition approximates to Ca<sub>12</sub>Al<sub>2</sub>Si<sub>18</sub>O<sub>69</sub>H<sub>36</sub>, and the X-ray diffraction patterns can be referred to an <italic>A</italic>-centred monoclinic pseudo-cell with <italic>a</italic> 17&#x00B7;07, <italic>b</italic> 3&#x00B7;65, <italic>c</italic> 27&#x00B7;9 &#x00C5;, &#x03B2; 114&#x00B7;1&#x00B0;, <italic>Z</italic> = I. In the true cell <italic>b</italic> is certainly, and <italic>a</italic> and <italic>c</italic> probably, doubled. Small, reversible changes in pseudo-cell parameters occur on heating below 200 &#x00B0;C, and parameters found by electron diffraction differ slightly from those found with X-rays, presumably due to shrinkage on dehydration in the high vacuum of the electron microscope. An earlier report that tacharanite changes into a mixture of tobermorite and gyrolite on standing in air is not confirmed. Tacharanite shows some important resemblances to tobermorite, but there are also significant differences.</p></abstract>
</article-meta>
</front>
</article>
