Pinalite, new lead tungsten chloride mineral from the Mammoth Mine, Pinal County, Arizona
Pinalite, Pb3WO5Cl2 is orthorhombic, A2aa or Amaa, with a 11.073(5), b 13.086(8), c 5.624(3) Angstrom, Z = 4; the strongest lines in the X-ray powder-diffraction pattern are 2.926(10), 3.778(9), 1.642(5), 3.284(4), 2.814(4). Pinalite occurs as exceedingly rare, bright yellow, acicular, bladed crysta...
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| Veröffentlicht in: | The American mineralogist 1989-08, Vol.74 (7-8), p.934-935 |
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| container_title | The American mineralogist |
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| creator | Dunn, Pete J Grice, Joel Denison Bideaux, Richard A |
| description | Pinalite, Pb3WO5Cl2 is orthorhombic, A2aa or Amaa, with a 11.073(5), b 13.086(8), c 5.624(3) Angstrom, Z = 4; the strongest lines in the X-ray powder-diffraction pattern are 2.926(10), 3.778(9), 1.642(5), 3.284(4), 2.814(4). Pinalite occurs as exceedingly rare, bright yellow, acicular, bladed crystals (0.03 times 0.01 times 0.2 mm in size), associated with leadhillite, cerussite and other minerals at the Mammoth mine, Pinal County, Arizona. The name is for the county in which the new mineral occurs. |
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Pinalite occurs as exceedingly rare, bright yellow, acicular, bladed crystals (0.03 times 0.01 times 0.2 mm in size), associated with leadhillite, cerussite and other minerals at the Mammoth mine, Pinal County, Arizona. The name is for the county in which the new mineral occurs.</description><identifier>ISSN: 0003-004X</identifier><identifier>EISSN: 1945-3027</identifier><language>eng</language><publisher>Mineralogical Society of America</publisher><subject>Arizona ; chemical composition ; chlorides ; crystal structure ; formula ; halides ; lead-tungsten chlorides ; Mammoth Mine ; mineral data ; mineralogy ; minerals ; new minerals ; nonsilicates ; Pinal County Arizona ; pinalite ; south-central Arizona ; United States ; X-ray diffraction data</subject><ispartof>The American mineralogist, 1989-08, Vol.74 (7-8), p.934-935</ispartof><rights>GeoRef, Copyright 2020, American Geosciences Institute. Reference includes data from Mineralogical Abstracts, United Kingdom @Twickenham @GBR @United Kingdom</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,776,780</link.rule.ids></links><search><creatorcontrib>Dunn, Pete J</creatorcontrib><creatorcontrib>Grice, Joel Denison</creatorcontrib><creatorcontrib>Bideaux, Richard A</creatorcontrib><title>Pinalite, new lead tungsten chloride mineral from the Mammoth Mine, Pinal County, Arizona</title><title>The American mineralogist</title><description>Pinalite, Pb3WO5Cl2 is orthorhombic, A2aa or Amaa, with a 11.073(5), b 13.086(8), c 5.624(3) Angstrom, Z = 4; the strongest lines in the X-ray powder-diffraction pattern are 2.926(10), 3.778(9), 1.642(5), 3.284(4), 2.814(4). Pinalite occurs as exceedingly rare, bright yellow, acicular, bladed crystals (0.03 times 0.01 times 0.2 mm in size), associated with leadhillite, cerussite and other minerals at the Mammoth mine, Pinal County, Arizona. The name is for the county in which the new mineral occurs.</description><subject>Arizona</subject><subject>chemical composition</subject><subject>chlorides</subject><subject>crystal structure</subject><subject>formula</subject><subject>halides</subject><subject>lead-tungsten chlorides</subject><subject>Mammoth Mine</subject><subject>mineral data</subject><subject>mineralogy</subject><subject>minerals</subject><subject>new minerals</subject><subject>nonsilicates</subject><subject>Pinal County Arizona</subject><subject>pinalite</subject><subject>south-central Arizona</subject><subject>United States</subject><subject>X-ray diffraction data</subject><issn>0003-004X</issn><issn>1945-3027</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1989</creationdate><recordtype>article</recordtype><sourceid/><recordid>eNotjstKxDAUQIMoWEf_IXtbuEn6yF0OxRfMoAsFXZWYxzRDm0CTYdCvd1BXZ3HgcM5IwbBuKgG8OycFAIgKoH6_JFcp7QE4Fw0W5OPFBzX5bEsa7JFOVhmaD2GXsg1Uj1NcvLF09sEuaqJuiTPNo6VbNc8xj3R7EiX9bdA-HkL-Kul68d8xqGty4dSU7M0_V-Tt_u61f6w2zw9P_XpTKc54rriWDHSLgIohA0ChhOZMC-Vko5TUaLnksoYGWOs6wNY5DhqN0w2aTyNW5Pavu7MxaW-Dtse4TGbYx8Ny-koDQ4kDdBJbKX4AWw1Rcw</recordid><startdate>198908</startdate><enddate>198908</enddate><creator>Dunn, Pete J</creator><creator>Grice, Joel Denison</creator><creator>Bideaux, Richard A</creator><general>Mineralogical Society of America</general><scope/></search><sort><creationdate>198908</creationdate><title>Pinalite, new lead tungsten chloride mineral from the Mammoth Mine, Pinal County, Arizona</title><author>Dunn, Pete J ; Grice, Joel Denison ; Bideaux, Richard A</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a212t-2c810c6909a1910093a3c21c3af85aa8c9e2828405016f7096ff20c9dfc59dbd3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1989</creationdate><topic>Arizona</topic><topic>chemical composition</topic><topic>chlorides</topic><topic>crystal structure</topic><topic>formula</topic><topic>halides</topic><topic>lead-tungsten chlorides</topic><topic>Mammoth Mine</topic><topic>mineral data</topic><topic>mineralogy</topic><topic>minerals</topic><topic>new minerals</topic><topic>nonsilicates</topic><topic>Pinal County Arizona</topic><topic>pinalite</topic><topic>south-central Arizona</topic><topic>United States</topic><topic>X-ray diffraction data</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Dunn, Pete J</creatorcontrib><creatorcontrib>Grice, Joel Denison</creatorcontrib><creatorcontrib>Bideaux, Richard A</creatorcontrib><jtitle>The American mineralogist</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Dunn, Pete J</au><au>Grice, Joel Denison</au><au>Bideaux, Richard A</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Pinalite, new lead tungsten chloride mineral from the Mammoth Mine, Pinal County, Arizona</atitle><jtitle>The American mineralogist</jtitle><date>1989-08</date><risdate>1989</risdate><volume>74</volume><issue>7-8</issue><spage>934</spage><epage>935</epage><pages>934-935</pages><issn>0003-004X</issn><eissn>1945-3027</eissn><abstract>Pinalite, Pb3WO5Cl2 is orthorhombic, A2aa or Amaa, with a 11.073(5), b 13.086(8), c 5.624(3) Angstrom, Z = 4; the strongest lines in the X-ray powder-diffraction pattern are 2.926(10), 3.778(9), 1.642(5), 3.284(4), 2.814(4). Pinalite occurs as exceedingly rare, bright yellow, acicular, bladed crystals (0.03 times 0.01 times 0.2 mm in size), associated with leadhillite, cerussite and other minerals at the Mammoth mine, Pinal County, Arizona. The name is for the county in which the new mineral occurs.</abstract><pub>Mineralogical Society of America</pub><tpages>2</tpages></addata></record> |
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| ispartof | The American mineralogist, 1989-08, Vol.74 (7-8), p.934-935 |
| issn | 0003-004X 1945-3027 |
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| source | EZB-FREE-00999 freely available EZB journals; Free Full-Text Journals in Chemistry |
| subjects | Arizona chemical composition chlorides crystal structure formula halides lead-tungsten chlorides Mammoth Mine mineral data mineralogy minerals new minerals nonsilicates Pinal County Arizona pinalite south-central Arizona United States X-ray diffraction data |
| title | Pinalite, new lead tungsten chloride mineral from the Mammoth Mine, Pinal County, Arizona |
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