Hrabakite, Ni9PbSbS8, a new member of the hauchecornite group from Pribram, Czech Republic

被引:5
|
作者
Sejkora, Jiri [1 ]
Skacha, Pavel [1 ,2 ]
Plasil, Jakub [3 ]
Dolnicek, Zdenek [1 ]
Ulmanova, Jana [1 ]
机构
[1] Natl Museum, Dept Mineral & Petrol, Cirkusova 1740, Prague 19300 9, Horni Podernice, Czech Republic
[2] Min Museum Pribram, Hynka Klicky Pl 293, Pribram 26101 6, Czech Republic
[3] ASCR, Inst Phys, Vvi, Slovance 1999-2, Prague 18221 8, Czech Republic
关键词
hrabakite; new mineral; hauchecornite group; crystal structure; uranium deposit; Pribram; Czech Republic; CRYSTAL-STRUCTURE; MINERALS; SYSTEM;
D O I
10.1180/mgm.2021.1
中图分类号
P57 [矿物学];
学科分类号
070901 ;
摘要
The new mineral hrabakite (IMA2020-034) was found in siderite-sphalerite gangue with minor dolomite-ankerite at the dump of shaft No. 9, one of the mines in the abandoned Pribram uranium and base-metal district, central Bohemia, Czech Republic. Hrabakite is associated with Pb-rich tucekite, Hg-rich silver, stephanite, nickeline, millerite, gersdorffite, sphalerite and galena. The new mineral occurs as rare prismatic crystals up to 120 mu m in size and allotriomorphic grains. Hrabakite is grey with a brownish tint. Mohs hardness is ca. 5-6; the calculated density is 6.37 g.cm(-3). In reflected light, hrabakite is grey with a brown hue. Bireflectance is weak and pleochroism was not observed. Anisotropy under crossed polars is very weak (brownish tints) to absent. Internal reflections were not observed. Reflectance values of hrabakite in air (R-min-R-max, %) are: 39.6-42.5 at 470 nm, 45.0-47.5 at 546 nm, 46.9-49.2 at 589 nm and 48.9-51.2 at 650 nm). The empirical formula for hrabakite, based on electron-microprobe analyses (n = 11), is (Ni8.91Co0.09Fe0.03)(9.03)(Pb0.94Hg0.04)(0.98)(Sb0.91As0.08)(0.99)S-7.99. The ideal formula is Ni9PbSbS8, which requires Ni 47.44, Pb 18.60, Sb 10.93 and S 23.03, total of 100.00 wt.%. Hrabakite is tetragonal, P4/mmm, a = 7.3085(4), c = 5.3969(3) angstrom, with V = 288.27(3) angstrom(3) and Z = 1. The strongest reflections of the calculated powder X-ray diffraction pattern [d, A (I)(hkl)] are: 3.6543(57)(200); 3.2685(68)(210); 2.7957(100)(211); 2.3920(87)(112); 2.3112(78)(310); 1.8663(74)(222); and 1.8083(71)(302). According to the single-crystal X-ray diffraction data (R-int = 0.0218), the unit cell of hrabakite is undoubtedly similar to the cell reported for tucekite. The structure contains four metal cation sites, two Sb (Sb1 dominated by Pb2+) and two Ni (with minor Co2+ content) sites. The close similarity in metrics between hrabakite and tucekite is due to similar bond lengths of Pb-S and Sb-S pairs. Hrabakite is named after Josef Hrabak, the former professor of the Pribram Mining College.
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页码:189 / 196
页数:8
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