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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.1960.032.248.02</article-id>
<title-group>
<article-title>Electron-Optical Data for Crystals of Scarbroite<xref ref-type="author-notes" rid="FN1">1</xref></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Brindley</surname>
<given-names>G. W.</given-names>
</name><degrees>M.Sc., Ph.D.</degrees></contrib>
<contrib contrib-type="author">
<name>
<surname>Comer</surname>
<given-names>J. J.</given-names>
</name><degrees>M.S.</degrees></contrib>
<aff>The Pennsylvania State University, University Park, Pennsylvania.</aff></contrib-group>
<author-notes>
<fn fn-type="other" id="FN1"><label>1</label><p>Contribution No. 59-21 from the college of Mineral Industries, The Pennsylvania State University, University Park, Pa.</p></fn></author-notes>
<pub-date pub-type="ppub">
<month>3</month>
<year>1960</year>
</pub-date>
<volume>32</volume>
<issue>248</issue>
<fpage>363</fpage>
<lpage>365</lpage>
<copyright-statement>Copyright &#x00A9; 1960, The Mineralogical Society</copyright-statement>
<copyright-year>1960</copyright-year>
<abstract>
<title>Summary</title>
<p>Electron micrographs of scarbroite show thin platy crystals of about 1 &#x03BC; size, having rhombic outlines with angles 66&#x00B0; &#x00B1; 1&#x00B0; and 113&#x00B0; &#x00B1; 1&#x00B0;. Single-crystal electron-diffraction patterns show rectangular net patterns, with <italic>d</italic><sub>100</sub> = 9&#x00B7;90 &#x00C5;., <italic>d</italic><sub>010</sub> = 14&#x00B7;67 &#x00C5;., <italic>&#x03B3;</italic>* = 90&#x00B0; &#x00B1; 0&#x00B7;05&#x00B0;. Strong <italic>hk0</italic> reflections show a pseudohexagonal arrangement, but true symmetry is probably orthorhombic or monoclinic. Faces outlining rhombic forms are of type &#x007B;11<italic>l</italic>&#x007D;, &#x007B;1&#x00AF;1<italic>l</italic>&#x007D;.</p></abstract>
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