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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.1972.038.300.04</article-id>
<title-group>
<article-title>Some Chemical Data on Members of the Shoshonite Association</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Joplin</surname>
<given-names>Germaine A.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Kiss</surname>
<given-names>E.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Ware</surname>
<given-names>N. G.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Widdowson</surname>
<given-names>Jennifer R.</given-names>
</name></contrib>
<aff>Department of Geophysics and Geochemistry, Australian National University, Canberra, A.C.T., Australia</aff></contrib-group>
<pub-date pub-type="ppub">
<month>12</month>
<year>1972</year>
</pub-date>
<volume>38</volume>
<issue>300</issue>
<fpage>936</fpage>
<lpage>945</lpage>
<history>
<date date-type="received">
<day>20</day>
<month>1</month>
<year>1972</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1972, The Mineralogical Society</copyright-statement>
<copyright-year>1972</copyright-year>
<abstract>
<title>Summary</title>
<p>A number of minerals and residual glasses from absarokites, shoshonites, and latites have been analysed by electron probe.</p>
<p>Clinopyroxenes show very little iron-enrichment and these rocks are thus distinguished from tholeiites and alkali basalts.</p>
<p>Glasses from this group are also distinct from tholeiites and alkali basalts and occupy a separate field on a CaO-Na<sub>2</sub>O-K<sub>2</sub>O diagram.</p></abstract>
</article-meta>
</front>
</article>
