首页> 外文期刊>Mineralogical Magazine >Magnesioleydetite and stra beta mannite, two new uranyl sulfate minerals with sheet structures from Red Canyon, Utah
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Magnesioleydetite and stra beta mannite, two new uranyl sulfate minerals with sheet structures from Red Canyon, Utah

机译:Magnesioleydetite和Stra Beta Mannite,两种新的铀硫酸盐矿物质,带有红峡谷,犹他州的片状结构

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Magnesioleydetite (IMA2017-063), Mg(UO2)(SO4)(2)center dot 11H(2)O, and stra beta mannite (IMA2017-086), Al(UO2)(SO4)(2)F center dot 16H(2)O, are two new minerals from mines in Red Canyon, San Juan County, Utah, USA. Magnesioleydetite occurs in the Markey mine and stra beta mannite occurs in both the Markey and Green Lizard mines. Both minerals are secondary phases found in efflorescent crusts on the surfaces of mine walls. Magnesioleydetite occurs in irregular aggregates (to similar to 0.5 mm) of blades (to similar to 0.2 mm) exhibiting the following properties: transparent to translucent; pale green-yellow colour; vitreous lustre; white streak; non-fluorescent; brittle; Mohs hardness approximate to 2; irregular fracture; one perfect cleavage on {001}; and calculated density = 2.463 g/cm(3). stra beta mannite occurs in irregular aggregates (to similar to 0.5 mm) of equant crystals (to similar to 0.2 mm) exhibiting the following properties: transparent; light yellow-green colour; vitreous to greasy lustre; nearly white streak; bright greenish-blue fluorescence; somewhat brittle, Mohs hardness approximate to 1 1/2; irregular fracture; one good cleavage on {001}; measured and calculated densities of 2.20(2) and 2.173 g/cm(3), respectively; optically biaxial (-); alpha = 1.477(2), beta = 1.485(2) and gamma = 1.489(2) (white light); 2V(meas.)= 72(2)degrees; dispersion r > v (slight); orientation Y= b, X boolean AND c= 20 degrees (in obtuse beta); pleochroism with X= nearly colourless, Y= pate green-yellow and Z= tight green-yellow (X < Y < Z). The empirical formulas for magnesioleydetite and stra beta mannite are (Mg0.56Fe0.26Zn0.11Mn0.01)(Sigma 0.94)(U0.99O2)(S1.015O4)(2)center dot 11H(2)O and Al1.00Na0.16(U0.99O2)(S1.00O4)(2)[F-0.58(OH)(0.42)]center dot 16H(2)O, respectively. Magnesioleydetite is monoclinic, C2/c, a= 11.3513(3), b = 7.7310(2), c= 21.7957(15) angstrom, beta=102.387(7)degrees, V= 1868.19(16) angstrom(3) and Z= 4. stra beta mannite is monoclinic, C2/c, a = 11.0187(5), b = 8.3284(3), c= 26.6727(19) angstrom, beta= 97.426(7)degrees, V = 2427.2(2) and Z= 4. The structures of magnesioleydetite (R-1 = 0.016 for 2040 I > 2 sigma I reflections) and stra beta mannite (R-1 = 0.0343 for 2220 I > 2 sigma I reflections) each contain uranyl-sulfate sheets based on the protasite-anion topology.
机译:Magnesioleydetite(IMA2017-063),Mg(UO2)(SO 4)(2)中心点11H(2)O,和Straβ甘蓝(IMA2017-086),Al(UO2)(SO4)(2)F中心点16H( 2)o是来自美国圣胡安县,犹他州的红峡谷的矿山的两个新矿物质。 Magnesioleydetite发生在马基矿山,在马基和绿色蜥蜴地雷发生的运动员麦克风。两种矿物质都是在矿井表面上的渐裂式外壳中发现的二次阶段。镁吲哚甲块在不规则的聚集体(至类似于0.5mm)的叶片(类似于0.2mm),表现出以下性质:至半透明透明;淡绿色的颜色;玻璃体光泽;白色条纹;非荧光;脆;莫赫斯硬度近似为2;不规则的骨折; {001}的一个完美的裂解;并计算密度= 2.463g / cm(3)。在不规则的聚集体(与0.5mm)的刻度晶体(至类似于0.2mm)的不规则聚集体(至0.2mm)中出现,表现出以下性能:透明;淡黄绿色;玻璃体油腻的光泽;几乎是白条纹;明亮的绿色蓝色荧光;有点脆,莫赫硬度近似为1 1/2;不规则的骨折; {001}良好的裂解;测量和计算的密度为2.20(2)和2.173g / cm(3);光学双轴( - ); alpha = 1.477(2),beta = 1.485(2)和伽马= 1.489(2)(白光); 2V(MEAS。)= 72(2)度;分散r> v(轻微);方向Y = B,X Boolean和C = 20度(在overuse beta中);具有x =几乎无色的,y = Pate绿色黄色和z =纯绿色黄色(x 2 sigma I反射)和straβ甘蓝(R-1 = 0.0343,用于2220℃> 2 sigma I反射)各自含有基于的铀酰硫酸盐片protasite-Anion拓扑。

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