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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.1957.031.238.01</article-id>
<title-group>
<article-title>G&#x00F6;tzenite and Combeite, Two New Silicates from the Belgian Congo</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Sahama</surname>
<given-names>Th. G.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Hyt&#x00F6;nen</surname>
<given-names>Kai</given-names>
</name> <degrees>M.A.</degrees></contrib>
<aff>Institute of Geology, University of Helsinki, Finland</aff></contrib-group>
<pub-date pub-type="ppub">
<month>9</month>
<year>1957</year>
</pub-date>
<volume>31</volume>
<issue>238</issue>
<fpage>503</fpage>
<lpage>510</lpage>
<copyright-statement>Copyright &#x00A9; 1957, The Mineralogical Society</copyright-statement>
<copyright-year>1957</copyright-year>
<abstract>
<title>Summary</title>
<p>A nephelinite from the extinct volcano Mt. Shaberu, North Kivu, Belgian Congo, contains two new minerals: <italic>G&#x00F6;tzenite</italic> is triolinic with <italic>a</italic> 10&#x00B7;93, <italic>b</italic> 7&#x00B7;32, <italic>c</italic> 5&#x00B7;74 &#x00C5;, <italic>&#x03B1;</italic> 90&#x00B0;, <italic>&#x03B2;</italic> 100&#x00B0;, <italic>&#x03B3;</italic> 120&#x00B0;; the unit-cell contents approximate to (Ca,Na,Al)<sub>7</sub> (Si,Ti)<sub>5</sub>O<sub>15</sub>F<sub>3&#x00B7;5</sub>, and the optical constants are <italic>&#x03B1;</italic> 1&#x00B7;660, <italic>&#x03B2;</italic> 1&#x00B7;662, <italic>&#x03B3;</italic> 1&#x00B7;670, 2V<sub><italic>&#x03B3;</italic></sub> 52&#x00B0;; sp.gr. 3&#x00B7;138. G&#x00F6;tzenite is related to the rinkite series, and, less closely, to wollastonite and pectolite. <italic>Combeite</italic> is rhombohedral, space-group <italic>R</italic>3<italic>m</italic>, <italic>R</italic>32, or <italic>R&#x00AF;3m, a</italic> 10&#x00B7;43, <italic>c</italic> 13&#x00B7;14 &#x00C5;., the unit cell containing approximately 3[Na<sub>4</sub>(Ca,Al,Fe)<sub>3</sub>Si<sub>6</sub>O<sub>15</sub>(O,OH,F)<sub>2</sub>]; optically uniaxial positive, &#x03B5; = &#x03C9; = 1&#x00B7;598&#x00B1;0&#x00B7;002; sp.gr. 2&#x00B7;844.</p></abstract>
</article-meta>
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