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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.1968.036.282.10</article-id>
<title-group>
<article-title>Compact Chlorite Associated with Lizardite from New South Wales, Australia</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Golding</surname>
<given-names>H. G.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Bayliss</surname>
<given-names>P.</given-names>
</name></contrib>
<aff>School of Applied Geology, The University of New South Wales</aff></contrib-group>
<pub-date pub-type="ppub">
<month>6</month>
<year>1968</year>
</pub-date>
<volume>36</volume>
<issue>282</issue>
<fpage>825</fpage>
<lpage>831</lpage>
<history>
<date date-type="received">
<day>10</day>
<month>10</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>Segregations of compact chlorite from ultramafic belts in New South Wales have been examined using chemical, X-ray, differential thermal, and electronprobe techniques. The chlorites vary from pennine to sheridanite. Some segregations occupy the central zone in metasomatic sequences of altered chromite, chlorite, and lizardite; but others may have formed at junctions of serpentinite and rodingite.</p></abstract>
</article-meta>
</front>
</article>
