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<article article-type="research-article">
<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.1968.036.281.04</article-id>
<title-group>
<article-title>Further Discussion of Framework Structures Built from Four- and Eight-Membered Rings</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Smith</surname>
<given-names>J. V.</given-names>
</name>
<aff>Department of the Geophysical Sciences, University of Chicago, Chicago, Illinois 60637, U.S.A.</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>3</month>
<year>1968</year>
</pub-date>
<volume>36</volume>
<issue>281</issue>
<fpage>640</fpage>
<lpage>642</lpage>
<history>
<date date-type="received">
<day>16</day>
<month>8</month>
<year>1967</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1968, The Mineralogical Society</copyright-statement>
<copyright-year>1968</copyright-year>
<abstract>
<title>Summary</title>
<p>The classification of framework structures built from chains of four-membered rings of type UUDD is incomplete: there are two basic ways in which the chains can be cross-linked to form eight-membered rings. The first type of frame-work (already described) is extremely flexible, permitting the cavities to be either large or small; the second type is inflexible and the cavities are small. Feldspar belongs to the second type and had been incorrectly ascribed to the first type: paracelsian, harmotome, and gismondine had been correctly placed in the first group.</p></abstract>
</article-meta>
</front>
</article>
