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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.1973.039.301.05</article-id>
<title-group>
<article-title>The Crystal Chemistry of the Amphiboles. I: Refinement of the Crystal Structure of Ferrotschermakite</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Hawthorne</surname>
<given-names>F. C.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Grundy</surname>
<given-names>H. D.</given-names>
</name></contrib>
<aff>Dept. of Geology, McMaster University, Hamilton, Ontario, Canada</aff></contrib-group>
<pub-date pub-type="ppub">
<month>3</month>
<year>1973</year>
</pub-date>
<volume>39</volume>
<issue>301</issue>
<fpage>36</fpage>
<lpage>48</lpage>
<history>
<date date-type="received">
<day>6</day>
<month>3</month>
<year>1972</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1973, The Mineralogical Society</copyright-statement>
<copyright-year>1973</copyright-year>
<abstract>
<title>Summary</title>
<p>Three-dimensional counter-diffractometer data and a full-matrix least-squares method have been used to refine the crystal structure of a ferrotschermakite in the space group <italic>C2/m</italic>. The chemical composition of the amphibole is <inline-formula><mml:math><mml:mrow><mml:msub><mml:mi>Na</mml:mi><mml:mrow><mml:mn>0</mml:mn><mml:mo>&#x00B7;</mml:mo><mml:mn>23</mml:mn></mml:mrow></mml:msub><mml:msub><mml:mi>K</mml:mi><mml:mrow><mml:mn>0</mml:mn><mml:mo>&#x00B7;</mml:mo><mml:mn>14</mml:mn></mml:mrow></mml:msub><mml:msub><mml:mi>Ca</mml:mi><mml:mrow><mml:mn>1</mml:mn><mml:mo>&#x00B7;</mml:mo><mml:mn>86</mml:mn></mml:mrow></mml:msub><mml:msub><mml:mi>Mg</mml:mi><mml:mrow><mml:mn>1</mml:mn><mml:mo>&#x00B7;</mml:mo><mml:mn>22</mml:mn></mml:mrow></mml:msub><mml:msubsup><mml:mrow><mml:mi>Fe</mml:mi></mml:mrow><mml:mrow><mml:mn>2</mml:mn><mml:mo>&#x00B7;</mml:mo><mml:mn>10</mml:mn></mml:mrow><mml:mrow><mml:mn>2</mml:mn><mml:mo>&#x002B;</mml:mo></mml:mrow></mml:msubsup><mml:msub><mml:mi>Mn</mml:mi><mml:mrow><mml:mn>0</mml:mn><mml:mo>&#x00B7;</mml:mo><mml:mn>02</mml:mn></mml:mrow></mml:msub><mml:msub><mml:mi>Ti</mml:mi><mml:mrow><mml:mn>0</mml:mn><mml:mo>&#x00B7;</mml:mo><mml:mn>10</mml:mn></mml:mrow></mml:msub><mml:msubsup><mml:mrow><mml:mi>Fe</mml:mi></mml:mrow><mml:mrow><mml:mn>0</mml:mn><mml:mo>&#x00B7;</mml:mo><mml:mn>30</mml:mn></mml:mrow><mml:mrow><mml:mn>3</mml:mn><mml:mo>&#x002B;</mml:mo></mml:mrow></mml:msubsup><mml:msub><mml:mi>Al</mml:mi><mml:mrow><mml:mn>1</mml:mn><mml:mo>&#x00B7;</mml:mo><mml:mn>30</mml:mn></mml:mrow></mml:msub><mml:msub><mml:mi>Al</mml:mi><mml:mrow><mml:mn>2</mml:mn><mml:mo>&#x00B7;</mml:mo><mml:mn>00</mml:mn></mml:mrow></mml:msub><mml:msub><mml:mi>Si</mml:mi><mml:mrow><mml:mn>6</mml:mn><mml:mo>&#x00B7;</mml:mo><mml:mn>00</mml:mn></mml:mrow></mml:msub><mml:msub><mml:mi>O</mml:mi><mml:mn>22</mml:mn></mml:msub><mml:msub><mml:mi>(OH)</mml:mi><mml:mn>2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> with cell parameters <italic>a</italic> 9&#x00B7;8179(7), <italic>b</italic> 18&#x00B7;1060(14), <italic>c</italic> 5&#x00B7;3314(5) &#x00C5;, and &#x03B2; 105&#x00B7;00(I). Cation site-occupancies were initially assigned by ionic-radius criteria and refined with the constraint that the sum total of the site-occupancies be equal to the chemical analysis.</p>
<p>The <italic>A</italic>-site shows positional and substitutional disorder and can be better represented by two sites, one on the mirror plane and the other on the 2-fold axis.</p>
<p>Unit weights were used throughout the refinement and the final <italic>R</italic>-factor for 1207 observed nonequivalent reflections was 4&#x00B7;5 %.</p></abstract>
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