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首页> 外文期刊>Journal of mineralogical and petrological sciences >Takanawaite-(Y), a new mineral of the M-type polymorph with Y(Ta,Nb)O4 from Takanawa Mountain, Ehime Prefecture, Japan
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Takanawaite-(Y), a new mineral of the M-type polymorph with Y(Ta,Nb)O4 from Takanawa Mountain, Ehime Prefecture, Japan

机译:Takanawaite-(Y),一种来自日本爱媛县Takanawa山的Y(Ta,Nb)O 4 的 M 型多晶型新矿物

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Takanawaite-(Y), a new mineral of the M -type polymorph with an generalized formula of Y(Ta,Nb)O_(4), is identified from Takanawa Mountain, Ehime Prefecture, Japan. It is dark brown in color and occurs as a single crystal with a tabular habit (up to 5 mm) or a radial aggregate of fine crystals. The hardness is 5 1/2 on Mohs scale. The empirical formula of takanawaite-(Y) is (Y_(0.75)Dy_(0.08)Yb_(0.05)Gd_(0.02)U_(0.03)Ti_(0.02)Fe_(0.02))_(Σ0.97)(Ta_(0.57)Nb_(0.45))_(Σ1.02)O_(4), leading to a simplified formula of Y(Ta,Nb)O_(4). The Ta/(Ta + Nb) ratio varies between 0.55 and 0.57. Takanawaite-(Y) naturally occurs in a submetamict state, and a heating treatment is required to determine the crystal structure. The heating experiment revealed the consistency of takanawaite-(Y) and its M -type polymorph. The mineral crystallizes in a monoclinic M -type structure with a space group I2/a , unit cell parameters a = 5.3182(8), b = 10.9583 (13), c = 5.0595 (7) ?, β = 94.993(14)°, and V = 293.74(7) ?~(3), and Z = 4, with a calculated density 6.97 g/cm~(3). The eight strongest lines in the powder XRD pattern [d (?), (I/I_(0) ), hkl ] are 3.1334 (100) 121, 2.9525 (85) 121, 2.7391 (29) 040, 2.6494 (21) 200, 1.9115 (24) 202, 1.9050 (39) 240, 1.8546 (26) 042, and 1.5681 (19) 242. Takanawaite-(Y) is a distinct mineral compared to iwashiroite-(Y), yttrotantalite-(Y), and formanite-(Y).
机译:Takanawaite-(Y)是一种新的M型多晶型矿物,其通式为Y(Ta,Nb)O_(4),是从日本爱媛县的Takanawa山中鉴定出来的。它为深棕色,以具有片状习性(最大5毫米)的单晶或细晶体的放射状聚集体形式出现。莫氏硬度为5 1/2。 takanawaite-(Y)的经验公式为(Y_(0.75)Dy_(0.08)Yb_(0.05)Gd_(0.02)U_(0.03)Ti_(0.02)Fe_(0.02))_(Σ0.97)(Ta_(0.57) )Nb_(0.45))_(Σ1.02)O_(4),从而得出Y(Ta,Nb)O_(4)的简化公式。 Ta /(Ta + Nb)比在0.55至0.57之间变化。 Takanawaite-(Y)自然存在于亚半金属状态,需要进行热处理才能确定其晶体结构。加热实验揭示了高岭土-(Y)及其 M-型多晶型物的稠度。矿物以空间群 I2 / a的单斜M型结构结晶,晶胞参数 a = 5.3182(8), b = 10.9583(13), c = 5.0595(7)θ,β= 94.993(14)°,V = 293.74(7)θ〜(3),Z = 4,计算出的密度为6.97g / cm 2()。 3)。粉末XRD图谱中最强的8条线[ d(?),( I / I_(0)), hkl]是3.1334(100)121、2.9525(85)121、2.7391( 29)040,2.6494(21)200,1.9115(24)202,1.9050(39)240,1.8546(26)042和1.5681(19)242。Takanawaite-(Y)是与iwashiroite-(Y ),钇钛矿(Y)和锰铁矿(Y)。

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