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Grandviewite redefinition, new formula Cu.sub.3./sub.Al.sub.2./sub.(SO.sub.4./sub.)(OH).sub.10./sub.·H.sub.2./sub.O, and crystal-structure determination

  1. 1.
    SYSNO ASEP0563223
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleGrandviewite redefinition, new formula Cu3Al2(SO4)(OH)10·H2O, and crystal-structure determination
    Author(s) Sejkora, J. (CZ)
    Steciuk, Gwladys (FZU-D) ORCID
    Marquez-Zavalia, M.F. (AR)
    Plášil, Jakub (FZU-D) RID, ORCID
    Dolníček, Z. (CZ)
    Number of authors5
    Source TitleMineralogical Magazine - ISSN 0026-461X
    Roč. 86, č. 5 (2022), s. 730-742
    Number of pages13 s.
    Languageeng - English
    CountryGB - United Kingdom
    Keywordsgrandviewite ; redefinition ; Raman and infrared spectroscopy ; 3D electron diffraction ; crystal structure ; Capillitas mine ; Argentina
    Subject RIVDB - Geology ; Mineralogy
    OECD categoryMineralogy
    Method of publishingLimited access
    Institutional supportFZU-D - RVO:68378271
    UT WOS000836952200001
    EID SCOPUS85133696412
    DOI10.1180/mgm.2022.59
    AnnotationGrandviewite is redefined on the basis of a restudy of the holotype specimen from the Grandview mine, Arizona, USA, and additional specimens found in the Restauradora vein at the Capillitas mine, northwestern Argentina. Grandviewite from the Capillitas mine forms globular masses up to a couple of millimeters in diameter, formed by very thin platy to acicular lath-like crystals, greenish-pale blue in color, pleochroic (X = colorless, Y = very pale blue, Z = greenish-pale blue), with pale blue streak and silky to a satiny luster. Results of electron-microprobe study and crystal-structure determination lead to the new ideal formula Cu3Al2(SO4)(OH)10.H2O.
    WorkplaceInstitute of Physics
    ContactKristina Potocká, potocka@fzu.cz, Tel.: 220 318 579
    Year of Publishing2023
    Electronic addresshttps://doi.org/10.1180/mgm.2022.59
Number of the records: 1  

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