首页> 外文期刊>Mineralogical Magazine >Stefanweissite, (Ca,REE)(2)Zr-2(Nb,Ti)(Ti,Nb)(2)Fe2+O14, a new zirconolite-related mineral from the Eifel paleovolcanic region, Germany
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Stefanweissite, (Ca,REE)(2)Zr-2(Nb,Ti)(Ti,Nb)(2)Fe2+O14, a new zirconolite-related mineral from the Eifel paleovolcanic region, Germany

机译:Stefanwissite,(Ca,Ree)(2)Zr-2(Nb,Ti)(Ti,Nb)(2)Fe2 + O14,来自德国eifel古奥维州地区的新锆石相关矿物质

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摘要

The new mineral stefanweissite, IMA2018-020, was discovered in sanidinite volcanic ejecta from the Laach Lake (Laacher See) paleovolcano, Eifel region, Rhineland-Palatinate, Germany. Associated minerals are sanidine, nosean, biotite, augite, titanite, ferriallanite(La), magnetite, baddeleyite and a pyrochlore-group mineral. Stefanweissite is brown and reddish-brown, with adamantine lustre; the streak is light brown to yellow. It forms long-prismatic crystals up to 0.03 mm x 0.07 mm x 1.0 mm and acicular crystals up to 2 mm long and 0.02 mm thick typically combined in radiated aggregates in cavities in sanidinite. D-calc. = 5.254 g/cm(3). The mean refractive index calculated from the Gladstone-Dale equation is 2.260. The Raman spectrum shows the absence of hydrogen-bearing groups. The chemical composition is (electron microprobe, wt%): CaO 7.63, MnO 2.51, FeO 7.86, Al2O3 0.25, La2O3 2.28, Ce2O3 6.54, Pr2O3 1.01, Nd2O3 1.59, ThO2 3.71, UO2 L09, TiO2 17.32, ZrO2 28.03, HfO2 0.91, Nb2O5 19.96, total 99.69. The empirical formula based on 14 O atoms per formula unit is Ca-1.13(Ce0.33La0.12Nd0.08Pr0.05)(Sigma 0.58)Th0.12U0.03Mn0.29Fe0.91Al0.04Zr1.89Hf0.04Ti1.80Nb1.19O14. The simplified formula is (Ca,REE)(2)Zr-2 (Nb,Ti)(Ti,Nb)(2)Fe2+O14. Stefanweissite is orthorhombic, with space group Cmca. The unit-cell parameters are: a = 7.2896(4) angstrom, b = 14.1435(5) angstrom, c = 10.1713(4) angstrom and V = 1048.68(7) angstrom(3). The crystal structure was solved using single-crystal X-ray diffraction data. Stefanweissite is an analogue of zirconolite-30 with Nb dominant over Ti in one of two octahedral sites. The strongest lines of the powder X-ray diffraction pattern [d, angstrom (I, %) (hkl)] are: 2.983(100)(202), 2.897(71)(042), 1.828(38)(154, 400, 333), 1.793(25)(244), 1.767(16)(080), 1.517(10)(282), 1.187(19)(483, 1.11.3, 602). Type material is deposited in the collections of the Fersman Mineralogical Museum of the Russian Academy of Sciences, Moscow, Russia, with the registration number 5191/1.
机译:新的矿物质斯维坦IMA2018-020在Laach Lake(Laacher See)Paleovolcano,Eifel Region,莱茵兰 - 普法尔茨,德国的Sanidinite Volcanic喷射物中发现。相关矿物质是凝视,核心,生物烟灰,消逝,二岩,铁铝石(La),磁铁矿,Baddeleyite和柏林矿物。斯特凡司石是棕色和红褐色的,带有金刚石光泽;条纹浅棕色至黄色。它形成长达棱镜晶体,高达0.03mm×0.07mm×1.0mm,可直射晶体长达2mm长,厚度为0.02mm,通常在Sanidinite中的空腔中组合在辐射的聚集体中。 D-Calc。 = 5.254 g / cm(3)。来自Gladstone-Dale等式计算的平均折射率为2.260。拉曼光谱显示不存在含氢基团。化学成分是(电子微探针,WT%):CaO 7.63,MnO 2.51,FeO 7.86,Al2O3 0.25,La2O3 2.28,Ce2O3 6.54,PR2O3 1.01,Nd2O3 1.59,ThO2 3.71,UO2 L09,TiO2 17.32,ZrO2 28.03,HFO2 0.91 ,NB2O5 19.96,总计99.69。基于每配方单元14 O原子的经验配方是Ca-1.13(Ce0.33La0.12nd0.08pr0.05)(Sigma 0.58)Th0.12u0.03mn0.29Fe0.91Al0.04zR1.89HF0.04Ti1.80nb1.19o14。简化的公式是(Ca,Ree)(2)Zr-2(Nb,Ti)(Ti,Nb)(2)Fe2 + O14。 Stefanwessite是正交的,空间组cmca。单位 - 细胞参数是:A = 7.2896(4)埃,B = 14.1435(5)埃,C = 10.1713(4)埃和V = 1048.68(7)埃(3)。使用单晶X射线衍射数据进行晶体结构。 Stefanwissite是锆酮-30的类似物,其中Nb在两个八面体位点中的一个占TI的TI。粉末X射线衍射模式的最强线[D,Angstrom(I,%)(HKL)]是:2.983(100)(202),2.897(71)(042),1.828(38)(154,400 ,333),1.793(244)(244),1.767(16)(080),1.517(10)(282),1.187(19)(483,11.1.3,602)。型号材料归还俄罗斯俄罗斯莫斯科学院的Fersman矿物学博物馆的收藏品,注册号码5191/1。

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