Detailed Information on Publication Record
2017
Babanekite, Cu-3(AsO4)(2) center dot 8H(2)O, from Jachymov, Czech Republic - a new member of the vivianite group
PLÁŠIL, Jakub, Pavel ŠKÁCHA, Jiří SEJKORA, Radek ŠKODA, Milan NOVÁK et. al.Basic information
Original name
Babanekite, Cu-3(AsO4)(2) center dot 8H(2)O, from Jachymov, Czech Republic - a new member of the vivianite group
Authors
PLÁŠIL, Jakub (203 Czech Republic), Pavel ŠKÁCHA (203 Czech Republic), Jiří SEJKORA (203 Czech Republic), Radek ŠKODA (203 Czech Republic, guarantor, belonging to the institution), Milan NOVÁK (203 Czech Republic, belonging to the institution), František VESELOVSKY (203 Czech Republic) and Jan HLOUŠEK (203 Czech Republic)
Edition
Journal of Geosciences, Praha, Česká geologická společnost, 2017, 1802-6222
Other information
Language
English
Type of outcome
Článek v odborném periodiku
Field of Study
10504 Mineralogy
Country of publisher
Czech Republic
Confidentiality degree
není předmětem státního či obchodního tajemství
Impact factor
Impact factor: 1.415
RIV identification code
RIV/00216224:14310/17:00100332
Organization unit
Faculty of Science
UT WoS
000423277800005
Keywords in English
babanekite; new mineral; vivianite group; crystal structure; Jachymov
Změněno: 29/3/2018 09:58, Ing. Nicole Zrilić
Abstract
V originále
Babanekite, Cu-3(AsO4)(2) center dot 8H(2)O, a new member of the vivianite group was found in material originating from the Geister vein, Rovnost mine, Jachymov, Western Bohemia, Czech Republic. It occurs as a supergene alteration mineral in association with members of the lindackerite supergroup (veselovskyite, hlousekite, pradetite and lindackerite), lavendulan, gypsum and an X-ray amorphous Cu-Al-Si-O-H phase. Crystals of babanekite are pinkish to peach-colored, elongated, prismatic and up to 2 mm in length. They exhibit the forms {010}, {100}, {110}, {101} and less frequently also {001}. Crystals are transparent to translucent with a vitreous luster. The mineral has a light pinkish streak. Estimated Mohs hardness is between 1.5 and 2. The cleavage is perfect on {010}. The calculated density is 3.192 g/cm(3). Electron-microprobe analysis yielded CoO 8.89, NiO 4.06, CuO 15.31, ZnO 10.87, P2O5 0.16, As2O5 39.79, SO3 0.13, H2O 24.78 (calc.), total 103.99 wt.% giving the empirical formula (Cu1.12Zn0.78Co0.69Ni0.32)(Sigma 2.91)[(AsO4)(2.01)(PO4)(0.01)(SO4)(0.01)](Sigma 2.03) center dot 8H(2)O based on 16 O apfu. The ideal end-member formula of babanekite is Cu-3(AsO4)(2) center dot 8H(2)O, which requires CuO 38.95, As2O5 37.52, H2O 23.53, total 100.00 wt.%. Babanekite is monoclinic, C2/m, with a = 10.1729(3), b = 13.5088(4), c = 4.7496(1) angstrom, beta = 105.399(2)degrees, V = 629.28(3) angstrom(3) and Z = 2. The eight strongest X-ray powder diffraction lines are [d(obs) angstrom(I)(hkl)]: 7.936(11)(110), 6.743(100)(020), 3.231(14)(13-1), 2.715(11)(041), 2.3331(10)(15-1), 2.0819(5)(350), 1.6862(16)(080) and 1.6107(4)(55-1). The crystal structure of babanekite, refined to R-1 = 2.18 % for 864 unique observed reflections, confirmed that the atomic arrangement is similar to other members of the vivianite group of minerals. The mineral is named for Ing. Frantisek Babanek (1836-1910), Czech mining and geological expert, who worked in the Jachymov and Pribram mines.
Links
MUNI/A/1316/2015, interní kód MU |
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