<?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.1978.042.322.03</article-id>
<title-group>
<article-title>Tlapallite, a New Mineral from Moctezuma, Sonora, Mexico</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Williams</surname>
<given-names>S. A.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Duggan</surname>
<given-names>Marjorie</given-names>
</name></contrib>
<aff>Phelps Dodge Corporation, Douglas, Arizona 85607, U.S.A.</aff></contrib-group>
<pub-date pub-type="ppub">
<month>6</month>
<year>1978</year>
</pub-date>
<volume>42</volume>
<issue>322</issue>
<fpage>183</fpage>
<lpage>186</lpage>
<history>
<date date-type="received">
<day>25</day>
<month>10</month>
<year>1977</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1978, The Mineralogical Society</copyright-statement>
<copyright-year>1978</copyright-year>
<abstract>
<title>Summary</title>
<p>Tlapallite is a new mineral found in 1972 at the Bambollita (La Oriental) mine near Moctezuma, Sonora. Also recently found in old specimens from Tombstone, Arizona. Data for type (Mexican) material: Colour viridian green RHS-128A with pale streak, H = 3, <italic>D</italic><sub>calc</sub> = 5&#x00B7;05 g/cm<sup>3</sup>. Crystals monoclinic, class unknown. Indexing based on Ito method gave a cell: <italic>a</italic> = 11&#x00B7;97 &#x00C5;, <italic>b</italic> = 9&#x00B7;11, <italic>c</italic> = 15&#x00B7;66, <italic>&#x03B2;</italic> = 90 &#x00B0; 36&#x2032;. Strongest lines: 11&#x00B7;972 &#x00C5; (10), 2&#x00B7;985 (10), 3&#x00B7;540 (6), 5&#x00B7;946 (5), 2&#x00B7;887 (5), 4&#x00B7;731 (4), 3&#x00B7;372 (4), 3&#x00B7;282 (4). Similar data obtain for Tombstone. Chemical analysis for type material yielded the formula H<sub>6</sub>Ca<sub>2</sub>Cu<sub>3</sub>(SO<sub>4</sub>)(TeO<sub>3</sub>)<sub>4</sub>,TeO<sub>6</sub> with Te<sup>4+</sup>:Te<sup>6+</sup> = 4:1. However, analysis of the Tombstone material indicates a more general formula H<sub>6</sub>(Ca, Pb)<sub>2</sub>(Cu, Zn)<sub>3</sub>(SO<sub>4</sub>) (TeO<sub>3</sub>)<sub>4</sub>,TeO<sub>6</sub>. The better data from this material indicate Z = 4, <italic>D</italic><sub>calc</sub> = 5&#x00B7;465 vs <italic>D</italic><sub>meas</sub> = 5&#x00B7;38. Characterized by extreme birefringence, <italic>&#x03B1;</italic> = 1&#x00B7;815, <italic>&#x03B2;</italic> = <italic>&#x03B3;</italic> = 1&#x00B7;960; for Tombstone <italic>&#x03B1;</italic> = 1&#x00B7;955, <italic>&#x03B2;</italic> = <italic>&#x03B3;</italic> = 2&#x00B7;115.</p>
<p>Named from the Nahua word tlapalli, meaning paint, in allusion to its mode of occurrence at the type locality.</p></abstract>
</article-meta>
</front>
</article>
