학술논문

Slikite, Zn2Mg(CO3)2(OH)2·4H2O, a new Zn-Mg carbonate from Plavno, Jachymov ore district, Czech Republic
Document Type
Academic Journal
Source
European Journal of Mineralogy. 31(5-6):1047-1054
Subject
01C|Mineralogy - nonsilicates
Bohemia
carbonates
cell dimensions
Central Europe
chemical composition
crystal structure
Czech Republic
electron probe data
Europe
formula
hardness
hydrates
infrared spectra
Jachymov mining district
Karlovy Vary Czech Republic
metamorphic rocks
metasomatic rocks
mineral cleavage
mineral interlayer
morphology
new minerals
optical properties
physical properties
Plavno Mine
Raman spectra
refractive index
skarn
slikite
spectra
vugs
X-ray diffraction data
Language
English
ISSN
0935-1221
Abstract
Slikite, Zn2Mg(CO3)2(OH)2·4H2O is a new supergene post-mining mineral from the Jachymov (formerly St. Joachimsthal) ore district, Czech Republic, associated with brianyoungite, hexahydrite, hydromagnesite, nesquehonite, serpierite, smithsonite and a ktenasite-like mineral. It forms snow-white radial aggregates, up to 2 mm across, in vugs or on surfaces of fragments of skarn rocks. Individual crystals are very thin blades, elongated along [110] and flattened on {001}, up to 200 µm in length. Slikite has a white streak, a vitreous lustre, and does not fluoresce under either short- or long-wave ultraviolet light. Cleavage is perfect on {001}, the Mohs hardness is ∼2, and the fracture is uneven. The mineral is brittle, although thin blades (fibres) are slightly flexible. The calculated density is 2.613 g/cm3. Slikite is optically biaxial negative, the indices of refraction are α=1.50(1), β=1.55(1), γ=1.59(1) and 2Vmeas.=80(1)°. The mineral is triclinic, space group P-1, a=6.335(4), b=6.340(1), c=13.923(4)Å, α=99.985(7)°, β=92.74(1)°, γ=114.93(2)°, V=494.8(4)Å3, Z=2. The seven strongest lines in the X-ray powder diffraction pattern are [d (Å)/I(hkl)]: 13.575/100(001), 4.525/31(003), 3.573/2(113), 3.406/5(111), 2.996/3(113) and 2.773/3(112). The chemical analyses by electron microprobe yielded MgO 8.39, ZnO 46.28, CuO 0.05, MnO 0.68, CdO 0.04, CO2calc. 23.10, H2Ocalc. 23.65, total 102.19 wt%. The empirical formula on the basis of 12 O atoms per formula unit is Zn2.00(Mg0.79Zn0.17Mn0.04)Σ1.00(CO3)2(OH)2·4H2O. The crystal structure of Slikite was refined using synchrotron single-crystal data to Robs=0.094 for 1594 reflections with I > 3σ(I). The structure of Slikite is based on heteropolyhedral layers of composition [Zn4Mg(CO3)4(OH)4]2-, parallel to {001}, with interlayer H-bonded [Mg(H2O)6]2+ and H2O. Within the layers, [110] chains of corner-connected ZnO2(OH)2 tetrahedra share corners with Mg-centred octahedra. The two types of polyhedra are connected via CO3 groups. The Raman and infrared spectra of Slikite as well as tentative assignment of observed bands are given in this paper. The mineral is named in honour of the prominent Czech aristocrat Stepan Slik (1487-1526), founder of town St. Joachimsthal (now Jachymov).