<?xml version="1.0"?>
<!DOCTYPE article SYSTEM "journalpublishing.dtd">
<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.1976.040.315.11</article-id>
<title-group>
<article-title>Cookeite and Diaspore in the Back Creek Pyrophyllite Deposit Near Pambula, New South Wales</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Loughnan</surname>
<given-names>F. C.</given-names>
</name>
<aff>School of Applied Geology, University of New South Wales, Kensington, N.S.W., Australia</aff></contrib>
<contrib contrib-type="author">
<name>
<surname>Steggles</surname>
<given-names>K. R.</given-names>
</name>
<aff>Australian Industrial Refractories Ltd., Mayfield, N.S.W., Australia</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>9</month>
<year>1976</year>
</pub-date>
<volume>40</volume>
<issue>315</issue>
<fpage>765</fpage>
<lpage>772</lpage>
<history>
<date date-type="received">
<day>15</day>
<month>10</month>
<year>1975</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1976, The Mineralogical Society</copyright-statement>
<copyright-year>1976</copyright-year>
<abstract>
<title>Summary</title>
<p>The occurrence of cookeite, a di/trioctahedral chlorite of composition (Al<sub>3&#x00B7;95</sub>Fe<sub>0&#x00B7;02</sub>Mg<sub>0&#x00B7;01</sub>Li<sub>0&#x00B7;81</sub>)(Al<sub>0&#x00B7;74</sub>Si<sub>3&#x00B7;26</sub>)O<sub>10</sub>(OH)<sub>8</sub>, in the Back Creek pyrophyllite deposit near Pambula is described. The mineral is restricted to a relatively narrow zone near the centre of the deposit and although diaspore is also present in this zone the two have not been found in intimate association, it is concluded that the introduction of lithium has been the principal factor controlling development of the cookeite.</p></abstract>
</article-meta>
</front>
</article>
