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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.1977.041.317.04</article-id>
<title-group>
<article-title>Luetheite, Cu<sub>2</sub>Al<sub>2</sub>(AsO<sub>4</sub>)<sub>2</sub>(OH)<sub>4&#x00B7;</sub>H<sub>2</sub>O, a New Mineral from Arizona, Compared with Chenevixite</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Williams</surname>
<given-names>S. A.</given-names>
</name>
<aff>Phelps Dodge Corporation, Douglas, Arizona, U.S.A.</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>3</month>
<year>1977</year>
</pub-date>
<volume>41</volume>
<issue>317</issue>
<fpage>27</fpage>
<lpage>32</lpage>
<history>
<date date-type="received">
<day>22</day>
<month>3</month>
<year>1976</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1977, The Mineralogical Society</copyright-statement>
<copyright-year>1977</copyright-year>
<abstract>
<title>Summary</title>
<p>Luetheite was found at a small prospect in Santa Cruz County, Arizona, as crystals in vugs in rhyolite porphyry. A few specimens were found on the dump, none seen in place. Occurs in silicified porphyry (quartzsericite-alunite) with chenevixite and hematite. Crystals indian blue inclining to greenish, H = 3, <italic>D</italic><sub>meas</sub> = 4&#x00B7;28.</p>
<p>Crystals monoclinic <italic>2/m</italic> and tabular on <italic>a</italic> &#x007B;100&#x007D;, also a plane of distinct cleavage; other forms are &#x007B;110&#x007D;, &#x007B;140&#x007D;, &#x007B;011&#x007D;. Space group perhaps <italic>P</italic>2<sub>1</sub>/<italic>m</italic> with <italic>a</italic> = 14&#x00B7;743&#x00C5;, <italic>b</italic> = 5&#x00B7;093, <italic>c</italic> = 5&#x00B7;598, <italic>&#x03B2;</italic> = 101&#x00B0; 49&#x2032;; strongest lines are 3&#x00B7;498&#x00C5; (10), 310, 111; 7&#x00B7;208 (7), 200; 2&#x00B7;507 (5), 120, 510. Feebly pleochroic in pale blue in thin section, <italic>&#x03B3;</italic> = <italic>&#x03B2;</italic> &#x003E; <italic>&#x03B1;</italic>. Indices are <italic>&#x03B1;</italic> = 1&#x00B7;752, <italic>&#x03B2;</italic> = 1&#x00B7;773, <italic>&#x03B3;</italic> = 1&#x00B7;796; 2V<italic>&#x03B3;</italic> = 88&#x00B0; (calc.); dispersion is moderate &#x03BD; &#x003E; <italic>&#x03C1;</italic>. <italic>&#x03B1;</italic> &#x2225; [010], <italic>&#x03B3;</italic>: [001] 10&#x00B0; in obtuse <italic>&#x03B2;</italic>. Duplicate chemical analyses averaged CuO 28&#x00B7;9%, Al<sub>2</sub>O<sub>3</sub> 18&#x00B7;4%, As<sub>2</sub>O<sub>5</sub> 40&#x00B7;5%, H<sub>2</sub>O 9&#x00B7;3% giving 2[Cu<sub>2</sub>Al<sub>2</sub> (AsO<sub>4</sub>)<sub>2</sub>(OH)<sub>4</sub>&#x00B7;H<sub>2</sub>O].</p>
<p>Named for R. D. Luethe, geologist for Phelps Dodge Corporation. Chenevixite from Las Animas, Sonora, analysed to give Cu<sub>2</sub>Fe<sub>2</sub>(AsO<sub>4</sub>)<sub>2</sub>(OH)<sub>4</sub>&#x00B7;H<sub>2</sub>O. Powder data are close to luetheite, and the cell is monoclinic <italic>2/m</italic>, probably <italic>P</italic>2<sub>1</sub>/<italic>m</italic>, with <italic>a</italic> = 15&#x00B7;006A, <italic>b</italic> = 5&#x00B7;189, <italic>c</italic> = 5&#x00B7;724, <italic>&#x03B2;</italic> = 102&#x00B0;15. The measured specific gravity is 4&#x00B7;38, <italic>D</italic><sub>cale</sub>. = 4&#x00B7;59. Crystals tabular on <italic>a</italic> &#x007B;100&#x007D; with a habit very similar to luetheite. Indices are <italic>&#x03B1;</italic> = 1&#x00B7;92 , <italic>&#x03B2;</italic> = 1&#x00B7;96, <italic>&#x03B3;</italic> = 2&#x00B7;04, 2V<italic>&#x03B3;</italic><sub>cale</sub>. = 75&#x00B0;; <italic>&#x03B1;</italic> &#x2225; [100], <italic>&#x03B3;</italic> nearly &#x2225; [001].</p></abstract>
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