首页> 外文期刊>Journal of mineralogical and petrological sciences >Hizenite-(Y), Ca2Y6(CO3)11·14H2O, a new mineral in alkali olivine basalt from Mitsukoshi, Karatsu, Saga Prefecture, Japan
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Hizenite-(Y), Ca2Y6(CO3)11·14H2O, a new mineral in alkali olivine basalt from Mitsukoshi, Karatsu, Saga Prefecture, Japan

机译:菱铁矿-(Y),Ca 2 Y 6 (CO 3 11 ·14H 2 < / sub> O,一种来自日本佐贺县唐津市三越的碱性橄榄石玄武岩中的新矿物

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Hizenite-(Y), ideal formula Ca_(2)Y_(6)(CO_(3))_(11)·14H_(2)O, occurs in druse of alkali olivine basalt at Mitsukoshi, Karatsu, Saga Prefecture, Japan. It occurs as a platy crystal and forms spherical aggregates. Hizenite-(Y) closely associates with lokkaite-(Y), tengerite-(Y), and kimuraite-(Y). It is orthorhombic, a = 6.295(1) ?, b = 9.089(2) ?, c = 63.49(1) ?, V = 3632(1) ?~(3), Z = 4. Hizenite-(Y) is white in color with vitreous to silky luster. The density is 2.98 g/cm~(3) (calc), and there is a perfect cleavage on {001}. The strongest lines in the X-ray powder diffraction pattern are [d (I /I _(0)hkl ] 10.63 (100) 006, 6.384 (77) 0·0·10, 3.962 (51) 0·0·16, 3.821 (27) 029, 1·0·13, 2.060 (23) 306, 0·4·13, 15.57 (20) 004.
机译:理想的Ca_(2)Y_(6)(CO_(3))_(11)·14H_(2)O的Hizenite-(Y)发生在日本佐贺县唐津市三越的碱性橄榄石玄武岩中。它以板状晶体形式存在,并形成球形聚集体。菱铁矿(Y)与菱铁矿(Y),辉铁矿(Y)和小土质(Y)密切相关。它是正交的, a = 6.295(1)?, b = 9.089(2)?, c = 63.49(1)?, V = 3632(1)?〜(3 ),Z =4。Hizenite-(Y)为白色,具有玻璃至丝般的光泽。密度为2.98 g / cm〜(3)(计算值),{001}上有一个完美的解理。 X射线粉末衍射图中最强的线为[d(i / I _(0)hkl] 10.63(100)006,6.384(77)0·0· 10、3.962(51)0·0·16、3.821(27)029、1·0·13、2.060(23)306、0·4·13、15.57(20)004。

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