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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.1972.038.299.13</article-id>
<title-group>
<article-title>Coexisting Hornblende and Cummingtonite from the Khetri Copper Belt, Rajasthan, India</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Das Gupta</surname>
<given-names>S. P.</given-names>
</name>
<aff>Geological Survey of India, 5-5-449 Mukaramjahi Road, Hyderabad-1, A.P., India</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>9</month>
<year>1972</year>
</pub-date>
<volume>38</volume>
<issue>299</issue>
<fpage>890</fpage>
<lpage>893</lpage>
<history>
<date date-type="received">
<day>26</day>
<month>7</month>
<year>1971</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1972, The Mineralogical Society</copyright-statement>
<copyright-year>1972</copyright-year>
<abstract>
<title>Summary</title>
<p>Coexisting hornblende and cummingtonite in an amphibolite near Peliwali have been analysed. The rock formed by Fe-Mg addition and Ca removal from pre-existing amphibole quartzites within the altered wall rocks surrounding sulphide lodes. The amphibole compositions are controlled by the bulk composition of the rock. The Mg/(Mg+Fe<sup>2+</sup>) ratio of the hornblende (0&#x00B7;66) is only slightly higher than that of the cummingtonite (0&#x00B7;64).</p></abstract>
</article-meta>
</front>
</article>
