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Pampaloite, AuSbTe, a new mineral from Pampalo gold mine, Finland

机译:Pampgelite,Ausbte,芬兰桅杆金矿的新矿物质

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Pampaloite, AuSbTe, is a new mineral discovered in the Pampalo gold mine, 65 km east of Joensuu, Finland. It forms anhedral grains (up to similar to 20 mu m) intergrown with gold, frohbergite and altaite. Pampaloite is brittle and has a metallic lustre. Values of VHN25 lie between 245 and 295 kg/mm(2), with a mean value of 276 kg/mm(2), corresponding to a Mohs hardness of similar to 4-5 (measured on synthetic material). In plane-polarised light, pampaloite is white with medium to strong bireflectance, weak reflectance pleochroism from slightly pinkish brown to slightly bluish white (only visible in grains of synthetic material containing multiple orientations), and strong anisotropy, with blue to light brown rotation tints; it exhibits no internal reflections. Reflectance values of pampaloite in air (R-1, R-2 in %) are: 60.0, 62.5 at 470 nm, 62.5, 64.8 at 546 nm, 63.2, 65.6 at 589 nm and 63.7, 66.0 at 650 nm. Ten electron-microprobe analyses of natural pampaloite give an average composition: Au 44.13, Sb 27.44 and Te 28.74, total 100.31 wt.%, corresponding to the empirical formula Au1.00Sb1.00Te1.00 based on 3 atoms; the average of eleven analyses on synthetic pampaloite is: Au 44.03, Sb 27.26, and Te 29.08, total 100.38 wt.%, corresponding to Au0 .99Sb1.00Te1.01. The density, calculated on the basis of the empirical formula, is 9.33 g/cm(3). The mineral is monoclinic, space group C2/c, with a = 11.947(3), b = 4.481(1) angstrom, c = 12.335(3) angstrom, beta= 105.83(2)degrees, V = 635.3(3) angstrom(3) and Z = 8. The crystal structure was solved and refined from the single-crystal X-ray-diffraction data of synthetic AuSbTe. The pampaloite crystal structure can be considered as a monoclinic derivative of the CdI2 structure composed of [AuTe3Sb3] octahedra. The strongest lines in the powder X-ray diffraction pattern of synthetic pampaloite [d in angstrom (I) (hkl)] are: 4.846(24)(202), 3.825(18)(111), 2.978(100)(311), 2.968(50)(004), 2.242(25)(020), 2.144(55) (313), 2.063(33)(315) and 1.789(18)(024).
机译:Pampaloite是Ausbte,是在芬兰加合约州东部65公里处发现的Pampalo Gold Lime的新矿物质。它与金色,Frohbergite和Atraite相互作用,形成腹膜粒(最高达20亩)。 Pampaloite很脆,具有金属光泽。 VHN25的值位于245和295kg / mm(2)之间,平均值为276kg / mm(2),对应于类似于4-5的MoHS硬度(在合成材料上测量)。在平面偏振光下,Pampaloite是白色的中染色体,弱反射率灵感来自略带粉红色的棕色,略微蓝白色(仅在含有多种方向的合成材料谷物中可见),浅棕色旋转色调。 ;它没有内部反射。空气中Pampaloite的反射值(R-1,R-2中)是:60.0,62.5,在470nm,62.5,64.8,63.2,65.6,63.2,65.6,63.7,65.0,65.0,65.0,65.0,65.0,650nm。天然潘纳洛钛的十个电子 - 微探针分析是平均成分:Au 44.13,Sb 27.44和Te 28.74,总量为100.31重量%,对应于基于3个原子的经验式Au1.00sb1.00te1.00; Inthetic Pampaloite上11分析的平均值是:Au 44.03,Sb 27.26和Te 29.08,总量为100.38重量%,对应于Au0.99sb1.00te1.01。基于经验公式计算的密度为9.33g / cm(3)。矿物是单斜晶,空间组C2 / C,A = 11.947(3),B = 4.481(1)埃,C = 12.335(3)埃,β= 105.83(2)度,v = 635.3(3)埃(3)和Z = 8.从合成AUSBTE的单晶X射线 - 衍射数据求解并改进晶体结构。 Pampaloite晶体结构可以被认为是由octahedra的CDI2结构的单斜衍生物。合成蛋白粉末X射线衍射图中的最强线[Angrom(I)(I)(HKL)]是:4.846(24)(202),3.825(18)(111),2.978(100)(311) ,2.968(50)(004),2.242(25)(020),2.144(55)(313),2.063(31)(315)和1.789(18)(024)。

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