PLÁŠIL, Jakub, Jiří SEJKORA, Radek ŠKODA, Milan NOVÁK, Anatoly V KASATKIN, Pavel ŠKACHA, František VESELOVSKY, Kristýna FEJFAROVÁ a Petr ONDRUŠ. Hloušekite, (Ni,Co)Cu-4(AsO4)(2)(AsO3OH)(2)(H2O)(9), a new member of the lindackerite supergroup from Jachymov, Czech Republic. Mineralogical Magazine. London: Mineralogical Society, 2014, roč. 78, č. 5, s. 1341-1353. ISSN 0026-461X. Dostupné z: https://dx.doi.org/10.1180/minmag.2014.078.5.16.
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Základní údaje
Originální název Hloušekite, (Ni,Co)Cu-4(AsO4)(2)(AsO3OH)(2)(H2O)(9), a new member of the lindackerite supergroup from Jachymov, Czech Republic
Autoři PLÁŠIL, Jakub (203 Česká republika, garant), Jiří SEJKORA (203 Česká republika), Radek ŠKODA (203 Česká republika, domácí), Milan NOVÁK (203 Česká republika, domácí), Anatoly V KASATKIN (643 Rusko), Pavel ŠKACHA (203 Česká republika), František VESELOVSKY (203 Česká republika), Kristýna FEJFAROVÁ (203 Česká republika) a Petr ONDRUŠ (203 Česká republika).
Vydání Mineralogical Magazine, London, Mineralogical Society, 2014, 0026-461X.
Další údaje
Originální jazyk angličtina
Typ výsledku Článek v odborném periodiku
Obor 10500 1.5. Earth and related environmental sciences
Stát vydavatele Velká Británie a Severní Irsko
Utajení není předmětem státního či obchodního tajemství
Impakt faktor Impact factor: 2.026
Kód RIV RIV/00216224:14310/14:00079323
Organizační jednotka Přírodovědecká fakulta
Doi http://dx.doi.org/10.1180/minmag.2014.078.5.16
UT WoS 000348531400016
Klíčová slova anglicky hloušekite; new mineral; arsenate; lindackerite supergroup; lindackerite group; ondrusite group; crystal structure
Štítky AKR, rivok
Příznaky Mezinárodní význam, Recenzováno
Změnil Změnila: Ing. Andrea Mikešková, učo 137293. Změněno: 8. 4. 2015 15:25.
Anotace
Hloušekite, (Ni,Co)Cu-4(AsO4)(2)(AsO3OH)(2)(H2O)(9), is a new supergene arsenate mineral from the Geister vein (Rovnost mine), Jachymov (St Joachimsthal), Western Bohemia, Czech Republic. It was found along with veselovskyite, pradetite, lavendulan, arsenolite, babanekite and gypsum on the surface of strongly altered ore fragments containing dominant tennantite and chalcopyrite. Hlous. ekite forms thin, lath-like crystals, locally elongated reaching up to 3 mm across. It is transparent, has a pale green colour with vitreous lustre, has a greyish-white streak and it is very brittle with an uneven fracture. It does not fluoresce under shortwave or longwave ultraviolet radiation. Cleavage on {010} is perfect; the Mohs hardness is 2-3. The calculated density is 3.295 g cm(-3). Hlous. ekite is optically biaxial with alpha' = 1.653(2) and gamma' = 1.73. The estimated optical orientation is gamma' vs. elongation (c) = 14(1)degrees. In larger grains it is weakly to moderately pleochroic (alpha = colourless, gamma = pale green to green). Hlousekite is triclinic, space group P (1) over bar, a = 6.4010(6), b = 8.0041(6), c = 10.3969(14) angstrom, alpha = 85.824(8), beta = 79.873(9), gamma = 84.655(7)degrees and V = 521.23(10) angstrom(3), with Z = 1, a:b:c = 0.800: 1: 1.299. The eight strongest lines in the powder X-ray diffraction (XRD) pattern [ d in angstrom (I)(hkl)] are 10.211(100)(001), 7.974(9)(010), 3.984(6)(020), 3.656(5)(1 (1) over bar2), 3.631(5)(0 (2) over bar1), 3.241(5)(022), 3.145(5)(200) and 3.006(5)(210). Chemical analysis by electron microprobe yielded MgO 0.20, FeO 0.10, NiO 5.79, CoO 1.80, CuO 29.53, ZnO 0.66, Al2O3 0.14, P2O5 0.11, As2O5 45.01, H2O 17.71 (calc.), for a total of 101.05 wt.%. The resulting empirical formula, calculated by stoichiometry (9H(2)O + 2OH), obtained from the crystal structure, is (Ni0.79Co0.25)(Sigma 1.04)(Cu3.78Zn0.08Mg0.05Al0.03Fe0.01)(Sigma 3.95) (AsO4)(1. 98)(PO4)(0.02)(AsO3OH)(2.00)(H2O)(9.00). The ideal endmember formula, NiCu4(AsO4)(2)(AsO3OH)(2)(H2O)(9.00), requires NiO 7.23, CuO 30.81, As2O5 44.51, H2O 17.45, total 100.00 wt.%. The crystal structure of hlous. ekite was solved by charge flipping from single-crystal XRD data and refined to R-1 = 0.0599 for 1441 reflections with [I-obs > 3 sigma(I)]. Hlousekite is a new member of the lindackerite group (also including lindackerite, pradetite and veselovskyite) of the lindackerite supergroup. The ondrusite group of the lindackerite supergroup includes ondrus. ite, chudobaite, geigerite and klajite. The establishment of these two groups reflects the difference between the crystal structures of their members, mainly in the coordination environment of the Me cations.
VytisknoutZobrazeno: 1. 9. 2024 01:36