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<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.1956.031.233.04</article-id>
<title-group>
<article-title>Staurolite Twinning</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Hurst</surname>
<given-names>Vernon J.</given-names>
</name> <degrees>B.S., M.S., Ph.D.</degrees>
<xref ref-type="author-notes" rid="FN1">1</xref></contrib>
<contrib contrib-type="author">
<name>
<surname>Donnay</surname>
<given-names>J. D. H.</given-names>
</name> <degrees>E. M., Ph.D.</degrees></contrib>
<aff>The Johns Hopkins University, Baltimore 18, Maryland, U.S.A.</aff></contrib-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Donnay</surname>
<given-names>Gabrielle</given-names>
</name> <degrees>B.A., Ph.D.</degrees>
<aff>Geophysical Laboratory, Carnegie Institution of Washington, Washington, D.C., U.S.A.</aff></contrib></contrib-group>
<author-notes>
<fn fn-type="present-address" id="FN1"><label>1</label><p>Present address: Department of Mines, Mining, and Geology, 425 State Capitol, Atlanta, Georgia, U.S.A.</p></fn></author-notes>
<pub-date pub-type="ppub">
<month>6</month>
<year>1956</year>
</pub-date>
<volume>31</volume>
<issue>233</issue>
<fpage>145</fpage>
<lpage>163</lpage>
<copyright-statement>Copyright &#x00A9; 1956, The Mineralogical Society</copyright-statement>
<copyright-year>1956</copyright-year>
<abstract>
<title>Summary</title>
<p>The space group <italic>Ccmm</italic> of the accepted staurolite structure (7&#x00B7;82:16&#x00B7;52:5&#x00B7;63 kX 0&#x00B7;473:1:0&#x00B7;341, N&#x00E1;ray-Szab&#x00F3; 1929) is a pseudo-space group; the true one has no <italic>c</italic> glide plane. Staurolite is monoclinie pseudo-orthorhombie, as shown optically by horizontal dispersion and morphologically by unequal developments of forms <italic>r</italic>(201) and <italic>r&#x2032;</italic>(<inline-formula><mml:math><mml:mrow><mml:mover><mml:mn>2</mml:mn><mml:mo>&#x00AF;</mml:mo></mml:mover><mml:mn>01</mml:mn></mml:mrow></mml:math></inline-formula>). It has variable cell dimensions, 7&#x00B7;83&#x2013;7&#x00B7;95:16&#x00B7;50&#x2013;16&#x00B7;82:5&#x00B7;62 5&#x00B7;71 &#x00C5;., constant <italic>&#x03B2;</italic> 90&#x00B0; + 3&#x2032;, aspect <italic>C</italic>*, and probable space group <italic>C</italic>2/<italic>m</italic> (negative pyroelectric test). This leads to the prediction of a new type of twin, &#x2018;by high order merohedry&#x2019;, a penetration twin that simulates an orthorhombie single crystal. It is known (Friedel, 1922) that the 90&#x00B0;-cross can be accounted for by two different twin laws and the 60&#x00B0;-cross by five. The twin operations are respectively the pseudo-symmetry operations of a pseudo-tetragonal cell, obtained by transformation 010/003/100, and those of Mallard's pseudo-cube, resulting from transformation <inline-formula><mml:math><mml:mrow><mml:mn>013/0</mml:mn><mml:mover><mml:mn>1</mml:mn><mml:mo>&#x00AF;</mml:mo></mml:mover><mml:mn>3/300</mml:mn></mml:mrow></mml:math></inline-formula>. By precession methods more than one twin law is established for each type of cross: both laws [100]<sub>90&#x00B0;</sub> and [013]<sub>180&#x00B0;</sub> are found for 90&#x00B0;-crosses: [313]<sub>180</sub> and [102]<sub>120&#x00B0;</sub>, for 60&#x00B0;-crosses.</p></abstract>
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