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<article article-type="research-article">
<front>
<journal-meta>
<journal-id journal-id-type="archive">gsminmag</journal-id>
<journal-title>Clay Minerals</journal-title>
<abbrev-journal-title abbrev-type="full">Clay Minerals</abbrev-journal-title>
<issn pub-type="ppub">0009-8558</issn>
<publisher>
<publisher-name>Mineralogical Society</publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.1180/minmag.1975.040.310.02</article-id>
<title-group>
<article-title>Carlfriesite, H<sub>4</sub> Ca(TeO<sub>3</sub>)<sub>3</sub>, a New Mineral from Moctezuma, Sonora, Mexico</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Williams</surname>
<given-names>Sidney A.</given-names>
</name>
<aff>Phelps Dodge Corporation, Douglas, Arizona</aff></contrib>
<contrib contrib-type="author">
<name>
<surname>Gaines</surname>
<given-names>Richard V.</given-names>
</name>
<aff>Pottstown, Pennsylvania</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>6</month>
<year>1975</year>
</pub-date>
<volume>40</volume>
<issue>310</issue>
<fpage>127</fpage>
<lpage>130</lpage>
<history>
<date date-type="received">
<day>26</day>
<month>8</month>
<year>1974</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1975, The Mineralogical Society</copyright-statement>
<copyright-year>1975</copyright-year>
<abstract>
<title>Summary</title>
<p>Carlfriesite is a new species found in relative abundance at the Bambollita (now La Oriental) mine in the Sierra La Huerta near Moctezuma, Sonora. Colour primrose yellow (R.H.S. 4B) with pale yellow streak. H = 3 &#x00BD; <italic>D</italic><sub>meas</sub> = 6&#x00B7;3, <italic>D</italic><sub>calc</sub> = 5&#x00B7;93. Fair cleavage on &#x007B;010&#x007D;. Monoclinic with <italic>a</italic> 12&#x00B7;585 &#x00C5;, <italic>b</italic> 5&#x00B7;658, <italic>c</italic> 9&#x00B7;985, &#x03B2; 115&#x00B0; 35&#x2032;. Space group <italic>Cc</italic> or <italic>C2/c</italic>. Strongest lines are 3&#x00B7;167 (IO), 3&#x00B7;o82 (9B), 5&#x00B7;o63 (6), 2&#x00B7;832 (6), 3&#x00B7;369 (4), 4&#x00B7;825 (3), 2&#x00B7;698 (3), and 4&#x00B7;o89 (2). Feeble pleochroism in pale yellow with <italic>&#x03B3;</italic> &#x003E; <italic>&#x03B1;</italic> = <italic>&#x03B2;;</italic> <italic>&#x03B1;</italic> = 1&#x00B7;982 ,<italic>&#x03B2;</italic> = 2&#x00B7;095, <italic>&#x03B3;</italic> 2&#x00B7;19; 2V<sub>&#x03B1;</sub> = 79&#x00B0; calc. Occurs with cerussite and chlorargyrite in an oxidized assemblage derived from hessite, galena, and bornite.</p></abstract>
</article-meta>
</front>
</article>
