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)O_4 from Takanawa Mountain, Ehime Prefecture, Japan
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Takanawaite-(Y), a new mineral of the M-type polymorph with Y(Ta,Nb)O_4 from Takanawa Mountain, Ehime Prefecture, Japan

机译:Takanawaite-(Y),一种来自日本爱媛县Takanawa山的具有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 51/2 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) A, β = 94.993(14)°, and V= 293.74(7) A~3, and Z = 4, with a calculated density 6.97 g/cm~3. The eight strongest lines in the powder XRD pattern [d(A) (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:从日本爱媛县高轮山鉴定出高岭土-(Y),一种新的M型多晶型矿物,通式为Y(Ta,Nb)O_4。其颜色为深棕色,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51/2。 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,得到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)A,β= 94.993(14)° ,V = 293.74(7)A〜3,Z = 4,计算出的密度为6.97g / cm〜3。粉末XRD图谱中最强的8条线[d(A)(I / I_0),hkl)为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。与伊势雄岩(Y),钇铝铁矿(Y)和锰铁矿((Y) )。

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