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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.1922.019.97.04</article-id>
<title-group>
<article-title>Relation of the Crystal-Structure of Some Carbon Compounds to Those of Graphite and Diamond<xref ref-type="fn" rid="FN1">1</xref></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Bragg</surname>
<given-names>William H.</given-names><prefix>Sir</prefix>
</name><degrees>K.B.E., D.Sc., F.R.S.</degrees>
<aff>Quain Professor of Physics in University College, University of London</aff></contrib></contrib-group>
<author-notes>
<fn fn-type="other" id="FN1"><label>1</label><p>Fuller details with diagrams are given in a Presidential Address to the Physical Society: Sir W. H. Bragg, &#x2018;The structure of organic crystals.&#x2019; Proc. Phys. Soc., 1921, vol. 34 pp. 33&#x2013;50.</p></fn></author-notes>
<pub-date pub-type="ppub">
<month>6</month>
<year>1922</year>
</pub-date>
<volume>19</volume>
<issue>97</issue>
<fpage>316</fpage>
<lpage>318</lpage>
<copyright-statement>Copyright &#x00A9; 1922, The Mineralogical Society</copyright-statement>
<copyright-year>1922</copyright-year>
</article-meta>
</front>
</article>
