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<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.1968.036.284.01</article-id>
<title-group>
<article-title>Onoratoite,<xref ref-type="fn" rid="FN1">1</xref> a New Antimony Oxychloride from Cetine Di Cotorniano, Rosia (Siena, Italy)</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Belluomini</surname>
<given-names>G.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Fornaseri</surname>
<given-names>M.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Nicoletti</surname>
<given-names>M.</given-names>
</name></contrib>
<aff>Istituto di Geochimica, Universit&#x00E0; di Roma</aff></contrib-group>
<author-notes>
<fn fn-type="other" id="FN1"><label>1</label><p>This new mineral has been approved by the Commission on New Minerals and New Mineral Names of the International Mineralogical Association. Some members of the Commission suggested that the name should be onoratoite instead of onoratite and this suggestion has been accepted by the authors of this paper.</p></fn></author-notes>
<pub-date pub-type="ppub">
<month>12</month>
<year>1968</year>
</pub-date>
<volume>36</volume>
<issue>284</issue>
<fpage>1037</fpage>
<lpage>1044</lpage>
<history>
<date date-type="received">
<day>23</day>
<month>5</month>
<year>1968</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1968, The Mineralogical Society</copyright-statement>
<copyright-year>1968</copyright-year>
<abstract>
<title>Summary</title>
<p>Onoratoite, a new antimony oxychloride Sb<sub>8</sub>O<sub>11</sub>Cl<sub>2</sub> from the antimony mines of Cetine di Cotorniano, Rosia (Siena, Italy), is triclinic with lattice constants <italic>a</italic> 18&#x00B7;92, <italic>b</italic> 4&#x00B7;03, <italic>c</italic> 10&#x00B7;31 &#x00C5;, <italic>&#x03B1;</italic> &#x2243; <italic>&#x03B3;</italic> &#x2243; 90&#x00B0;, <italic>&#x03B2;</italic> 110&#x00B0;. Density 5&#x00B7;3 meas., 5&#x00B7;49 calc. The needle-like crystals are elongated on [010] and show as prominent form &#x007B;001&#x007D;. Other forms present are &#x007B;100&#x007D;, &#x007B;201&#x007D;, &#x007B;401&#x007D;, &#x007B;412&#x007D;.</p>
<p>The new mineral is optically biaxial negative, extinction angle small and variable from 0&#x00B0; to 14&#x00B0;. Orientation <italic>&#x03B2;</italic>:[100] <italic>ca.</italic> 8&#x00B0;; <italic>&#x03B1;</italic>:[001] <italic>ca.</italic> 12&#x00B0;; <italic>&#x03B3;</italic>:[010] 0 to 14&#x00B0;. Refractive indices are 2&#x00B7;26 &#x003E; <italic>&#x03B3;</italic> &#x003E; 2&#x00B7;23, 2&#x00B7;23 &#x003E; <italic>&#x03B2;</italic> &#x003E; 2&#x00B7;18. Birefringence <italic>&#x03B3;</italic>-<italic>&#x03B2;</italic> 0&#x00B7;024 (meas.).</p>
<p>The stability field of onoratoite has been investigated by systematic thermo-gravimetric and differential thermal analysis of antimony oxychlorides and by a direct study of equilibrium relationships in the system SbCl<sub>3</sub>-Sb<sub>2</sub>O<sub>3</sub>-HCl-H<sub>2</sub>O. The probable mechanism of formation of onoratoite is discussed.</p>
<p>Onoratoite is named in honour of the Italian mineralogist Ettore Onorato.</p></abstract>
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