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@article{1497279,
author = {Plášil, Jakub and Kampf, Anthony R and Sejkora, Jiří and Čejka, Jiří and Škoda, Radek and Tvrdý, Jaromír},
article_location = {Prague},
article_number = {3},
doi = {http://dx.doi.org/10.3190/jgeosci.267},
keywords = {horákite; new mineral; uranyl arsenate; crystal structure; topology; Jáchymov},
language = {eng},
issn = {1802-6222},
journal = {Journal of Geosciences},
title = {Horakite, a new hydrated bismuth uranyl-arsenate-phosphate mineral from Jachymov (Czech Republic) with a unique uranyl-anion topology},
url = {http://dx.doi.org/10.3190/jgeosci.267},
volume = {63},
year = {2018}
}
TY - JOUR
ID - 1497279
AU - Plášil, Jakub - Kampf, Anthony R - Sejkora, Jiří - Čejka, Jiří - Škoda, Radek - Tvrdý, Jaromír
PY - 2018
TI - Horakite, a new hydrated bismuth uranyl-arsenate-phosphate mineral from Jachymov (Czech Republic) with a unique uranyl-anion topology
JF - Journal of Geosciences
VL - 63
IS - 3
SP - 265-276
EP - 265-276
PB - Czech Geological Society
SN - 18026222
KW - horákite
KW - new mineral
KW - uranyl arsenate
KW - crystal structure
KW - topology
KW - Jáchymov
UR - http://dx.doi.org/10.3190/jgeosci.267
L2 - http://dx.doi.org/10.3190/jgeosci.267
N2 - Horákite, ideally (Bi7O7OH)[(UO2)4(PO4)2(AsO4)2(OH)2]·3.5H2O, is a new uranyl mineral discovered on a specimen originating from Jáchymov, Czech Republic (most probably from the Geister vein, Rovnost mine). It occurs as a su-pergene alteration mineral in association with phosphuranylite (overgrowing older metatorbernite–metazeunerite) in a quartz gangue with abundant tennantite. Horákite forms greenish-yellow to pale yellow prismatic crystals clustering to acicular aggregates, up to 1 mm across. Crystals are transparent to translucent with a vitreous luster. The mineral has a light yellow streak. Estimated Mohs’ hardness is ~2. The cleavage is perfect on {100}. The calculated density is 6.358 g/cm3. Horákite is optically biaxial (+), alpha =approx 1.81, beta =approx 1.84, gamma =approx 1.88 (measured in white light); 2Vobs. is 78(1)°, 2Vcalc. is 83°; non-pleochroic. The optical orientation is X = b, Z =approx.c. Electron-microprobe analysis yielded the empirical formula (Bi7.01Pb0.14)O7OH[(U1.01O2)4(P1.03O4)2(As0.74Si0.23O4)2(OH)2]·3.5H2O based on 37.5 O apfu. Horákite is monoclinic, C2/c, a = 21.374(2), b = 15.451(3), c = 12.168(2) A, beta = 122.26(1)° and V = 3398.1(10) A3, Z = 4. The eight strongest X-ray powder-diffraction lines are [dobs A(I)(hkl)]: 11.77(100)(110), 6.21(23)(–202), 5.55(23)(310, –112), 4.19(27)(–331), 3.54(61)( 510, –423), 3.29(20)( 331), 3.14(58)(241, 023) and 3.02(98)(150, 113, –533, mult.). The crystal structure refinement of horákite, refined to R = 5.95 % for 1774 unique observed reflections, revealed a novel sheet structure. It consists of topologically unique [(UO2)4(PO4)2(AsO4)2(OH)2] sheets (i.e., horákite topology), and an interstitial {(Bi7O7OH)(H2O)3.5} complex. Sheets result from the polymerization of UO7 bipyramids by sharing edges to form tetrameric units; tetrahedrally coordinated sites are linked to the UO7 both monodentately (T1 to U1) and bidentately (T2 to U2). The mineral is named after František Horák (1882–1919), the mining engineer in Jáchymov, and his grandson, Vladimír Horák (born 1964), an amateur mineralogist and expert on the mining history of the Jáchymov ore district.
ER -
PLÁŠIL, Jakub, Anthony R KAMPF, Jiří SEJKORA, Jiří ČEJKA, Radek ŠKODA a Jaromír TVRDÝ. Horakite, a new hydrated bismuth uranyl-arsenate-phosphate mineral from Jachymov (Czech Republic) with a unique uranyl-anion topology. \textit{Journal of Geosciences}. Prague: Czech Geological Society, 2018, roč.~63, č.~3, s.~265-276. ISSN~1802-6222. Dostupné z: https://dx.doi.org/10.3190/jgeosci.267.
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