<?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.1964.033.267.01</article-id>
<title-group>
<article-title>Mboziite, a New Sodic Amphibole End-Member</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Brock</surname>
<given-names>P. W. G.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Gellatly</surname>
<given-names>D. C.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>von Knorring</surname>
<given-names>O.</given-names>
</name></contrib>
<aff>Dept. of Geology, University of Leeds, Leeds 2</aff></contrib-group>
<pub-date pub-type="ppub">
<month>12</month>
<year>1964</year>
</pub-date>
<volume>33</volume>
<issue>267</issue>
<fpage>1057</fpage>
<lpage>1065</lpage>
<copyright-statement>Copyright &#x00A9; 1964, The Mineralogical Society</copyright-statement>
<copyright-year>1964</copyright-year>
<abstract>
<title>Summary</title>
<p>An amphibole occurring in the Mbozi syenite-gabbro complex in SW. Tanganyika approaches very closely to the theoretical end-member <inline-formula><mml:math><mml:mrow><mml:msub><mml:mi>Na</mml:mi><mml:mn>2</mml:mn></mml:msub><mml:mi>Ca</mml:mi><mml:msubsup><mml:mrow><mml:mi>Fe</mml:mi></mml:mrow><mml:mrow><mml:mn>3</mml:mn></mml:mrow><mml:mrow><mml:mo>&#x2025;</mml:mo></mml:mrow></mml:msubsup><mml:msubsup><mml:mrow><mml:mi>Fe</mml:mi></mml:mrow><mml:mrow><mml:mn>2</mml:mn></mml:mrow><mml:mrow><mml:mo>&#x2026;</mml:mo></mml:mrow></mml:msubsup><mml:msub><mml:mi>Al</mml:mi><mml:mn>2</mml:mn></mml:msub><mml:msub><mml:mi>Si</mml:mi><mml:mn>6</mml:mn></mml:msub><mml:msub><mml:mi>O</mml:mi><mml:mn>22</mml:mn></mml:msub><mml:msub><mml:mo>(</mml:mo><mml:mi>OH</mml:mi><mml:mo>)</mml:mo><mml:mn>2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>; it has <italic>&#x03B1;</italic> 1&#x00B7;705, pale to light yellow, <italic>&#x03B2;</italic> 1&#x00B7;713, deep blue-green, <italic>&#x03B3;</italic> 1&#x00B7;715, deep blue to green to black, with <italic>&#x03B3;</italic> &#x2016; [010] and <italic>&#x03B2;</italic> : [001] about 7 to 14&#x00B0;; absorption <italic>&#x03B3;</italic> &#x003E; <italic>&#x03B2;</italic> &#x226B; <italic>&#x03B1;</italic>, with the maximum absorption on (010) at 9 to 12&#x00B0; to [001]. The mineral shows anomalous bright orange-red interference colours and incomplete extinction in sections parallel to (010) even in monochromatic light. X-ray powder data are given. A very similar amphibole occurs in the Darkainle nepheline-syenite complex, Borama district, Somali Republic.</p></abstract>
</article-meta>
</front>
</article>
