Karpenkoite, Co3(V2O7)(OH)2•2H2O, a cobalt analogue of martyite from the Little Eva mine, Grand County, Utah, USA

被引:7
|
作者
Kasatkin, Anatoly V. [1 ]
Plasil, Jakub [2 ]
Pekov, Igor V. [3 ]
Belakovskiy, Dmitry I. [1 ]
Nestola, Fabrizio [4 ]
Cejka, Jiri [5 ]
Vigasina, Marina F. [3 ]
Zorzi, Federico [4 ]
Thorne, Brent
机构
[1] Russian Acad Sci, Fersman Mineral Museum, Moscow 119071, Russia
[2] Acad Sci Czech Republ, Inst Phys, Vvi, Na Slovance 2, Prague 18221 8, Czech Republic
[3] Moscow MV Lomonosov State Univ, Fac Geol, Moscow 119991, Russia
[4] Univ Padua, Dipartimento Geosci, I-35131 Padua, Italy
[5] Natl Museum, Dept Mineral & Petrol, Prague 19300 9, Czech Republic
基金
俄罗斯基础研究基金会;
关键词
karpenkoite; new mineral; cobalt divanadate; powder diffraction; Little Eva mine; Utah; CRYSTAL-STRUCTURE; X-RAY; VOLBORTHITE; DISTANCES; VANADATE;
D O I
10.3190/jgeosci.199
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Karpenkoite (IMA 2014-092), ideally Co-3(V2O7)(OH)(2)center dot 2H(2)O, is a new divanadate mineral species, the cobalt analogue of martyite, found at the Little Eva mine, Grand County, Utah, USA. It occurs on sandstone matrix in close association with martyite, quartz, gypsum, baryte, roscoelite and an unidentified Al vanadate. Karpenkoite is a secondary mineral formed during the post-mining oxidation of corvusite and montroseite in a moist environment at ambient temperatures. The new mineral occurs as lamellar crystals, coarsely hexagonal or irregular in shape, typically curved. The crystals form rose-like clusters or globular aggregates up to 0.2 mm across. Karpenkoite is orange with pale yellow-orange streak. It is transparent with a vitreous luster. The mineral is brittle, with laminated fracture and perfect cleavage on {001}. The calculated density is 3.415 g cm(-3). The mineral is optically uniaxial (+), with omega = 1.827(8) and epsilon = 1.843(8). The chemical composition of karpenkoite (wt. %, electron-microprobe data) is: MgO 0.05, CaO 0.26, MnO 1.39, CoO 33.22, NiO 2.02, CuO 0.28, ZnO 12.66, V(2)O(5)38.70, H2O (calc.) 11.61, total 100.19. The empirical formula, calculated on the basis of 11 O apfu, is (Co2.06Zn0.72Ni0.13Mn0.09Ca0.02Cu0.02Mg0.01)(Sigma 3.05)V1.98O7(OH)(2)center dot 2H(2)O. The Raman spectrum demonstrates symmetric stretching and bending vibrations of V5+O3 units and the O-H stretching and bending vibrations of the H2O molecules. The new mineral is trigonal, the most probable space group is P (3) over bar m1 (by analogy with its Zn analogue martyite), a = 6.016(4), c = 7.234(6)angstrom, V = 226.7(2)angstrom(3) and Z = 1. The strongest powder X-ray diffraction lines are [d(obs),angstrom(I)(hkl)]: 7.15(100)(001), 5.19(18)(010), 4.20(25)(101,011), 3.59(21)(002), 2.95(54)(012,102), 2.77(21)(111), 2.60(36)(200), and 2.44(33)(201,021). The new mineral is named in honor of the Russian mineralogist Vladimir Yu. Karpenko (b. 1965), an expert on the mineralogy of vanadium.
引用
收藏
页码:251 / 257
页数:7
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