Tsikourasite, Mo3Ni2P1+x (x < 0.25), a New Phosphide from the Chromitite of the Othrys Ophiolite, Greece

被引:6
|
作者
Zaccarini, Federica [1 ]
Bindi, Luca [2 ]
Ifandi, Elena [3 ,4 ]
Grammatikopoulos, Tassos [5 ]
Stanley, Chris [6 ]
Garuti, Giorgio [1 ]
Mauro, Daniela [7 ]
机构
[1] Univ Leoben, Dept Appl Geol Sci & Geophys, A-8700 Leoben, Austria
[2] Univ Firenze, Dipartimento Sci Terra, I-150121 Florence, Italy
[3] Univ Patras, Dept Geol, Sect Earth Mat, Patras 26500, Greece
[4] Univ Brunei Darussalam, Fac Sci Phys & Geol Sci, BE-1410 Gadong, Brunei
[5] SGS Canada Inc, 185 Concess St,PO 4300, Lakefield, ON K0L 2H0, Canada
[6] Nat Hist Museum, Dept Earth Sci, London SW7 5BD, England
[7] Univ Pisa, Dipartimento Sci Terra, I-56126 Pisa, Italy
来源
MINERALS | 2019年 / 9卷 / 04期
关键词
tsikourasite; phosphide; chromitite; Agios Stefanos mine; Othrys; ophiolite; Greece; CRYSTAL-STRUCTURE; 1ST OCCURRENCES; PHOSPHORUS; MINERALS; VOURINOS; COMPLEX; SYSTEM; PINDOS; ROCKS; AREA;
D O I
10.3390/min9040248
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
Tsikourasite, Mo3Ni2P1+x (x < 0.25), is a new phosphide discovered in a mantle-hosted podiform chromitite collected in the abandoned mine of Agios Stefanos (Othrys ophiolite), Central Greece. It forms tiny grains (from a few m up to about 80 m) and occurs as isolated grains or associated with other known minerals such as nickelphosphide and awaruite, and with undetermined minerals such as Ni-allabogdanite or Ni-barringerite and a V-sulphide. Tsikourasite is brittle and has a metallic luster. In plane-polarized light, tsikourasite is white yellow and it shows no bireflectance, anisotropism or pleochroism. Internal reflections were not observed, Reflectance values of tsikourasite in air (R in %) are: 55.7 at 470 nm, 56.8 at 546 nm, 57.5 at 589 nm and 58.5 at 650 nm. Five spot analyses of tsikourasite give the average composition: P 7.97, S 0.67, V 14.13, Fe 14.37, Co 7.59, Ni 23.9, and Mo 44.16, total 99.60 wt.%, corresponding to the empirical formula (Mo1.778V1.071Fe0.082Co0.069)(sigma 3.000)(Ni1.572Co0.428)(sigma 2.000)(P0.981S0.079)(sigma 1.060), on the basis of sigma(Mo +V + Fe + Co + Ni) = 5 apfu and taking into account the structural results. The simplified formula is Mo3Ni2P1+x (x < 0.25). The density, which was calculated based on the empirical formula and single-crystal data, is 9.182 g/cm(3). The mineral is cubic, space group F-43m, with a = 10.8215(5) angstrom and Z = 16. Although tsikourasite is similar in composition to those of monipite (MoNiP), polekhovskyite (MoNiP2), and the synthetic compound MoNiP2, all these phases are hexagonal and not cubic like tsikourasite. It exhibits the same structure as the cubic Mo3Ni2P1.18 compound [space group F-43m, a = 10.846(2) angstrom] synthesized at 1350 degrees C. The mineral and its name have been approved by the Commission of New Minerals, Nomenclature and Classification of the International Mineralogical Association (No. 2018-156). The mineral honors Professor Basilios Tsikouras of the Universiti Brunei Darussalam.
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页数:13
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