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首页> 外文期刊>Mineralogical Magazine >As-bearing new mineral species from Valletta mine, Maira Valley, Piedmont, Italy: III. Canosioite, Ba2Fe3+(AsO4)(2)(OH), description and crystal structure
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As-bearing new mineral species from Valletta mine, Maira Valley, Piedmont, Italy: III. Canosioite, Ba2Fe3+(AsO4)(2)(OH), description and crystal structure

机译:来自Valletta矿,Maira Valley,意大利皮埃蒙特的含量新的矿物质:III。 甘皂石,Ba2Fe3 +(ASO4)(2)(OH),描述和晶体结构

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THE new mineral species canosioite, ideally Ba2Fe3+(AsO4)(2)(OH), has been discovered in the dump of Valletta mine, Maim Valley, Cameo Province, Piedmont, Italy. Its origin is probably related to the reaction between ore minerals and hydrothermal fluids. It occurs in reddish-brown granules, subhedral millimetre-size crystals, with a pale yellow streak and vitreous lustre. Canosioite is associated with aegirine, baryte, calcite, hematite, bronze Mn-bearing muscovite, unidentified Mn oxides and unidentified arsenates. Canosioite is biaxial (+) with a = 84(2)degrees.It is weakly pleochroic with X= brownish yellow,Y = brown, Z = reddish brown Z > Y> X Canosioite is monoclinic, P21/m, with a= 7.8642(4), h= 6.1083(3), c = 9.1670(5) angstrom, beta =112.874(6)degrees, V= 405.73(4) angstrom(3) and Z= 2. Calculated density is 4.943 g cm(3). The seven strongest diffraction lines of the observed powder X-ray diffraction pattern are [d in angstrom, (I) (hkI)]: 3.713 (18)(111), 3.304 (100)(21 (1) over bar), 3.058 (31)(020), 3.047 (59)(103), 2.801 (73)(112), 2.337 (24)(220), 2.158 (24)(123). Electron microprobe analyses gave (wt.%): Na2O 0.06, MgO 0.43, CaO 0.02, NiO 0.02, CuO 0.03, SrO 0.42, BaO 49.36, PhO 1.69, Al2O3 1.25, Mn2O3 3.89, Fe2O3 6.95, Sb2O3 0.01, SiO2 0.03, P2O5 0.02, V2O5 10.88, As2O5 24.64, SO3 0.01, F 0.02, H2O 1.61 was calculated on the basis of 1 (OH,F,H2O) group per formula unit. Infrared spectroscopy confirmed the presence of OK The empirical formula calculated on the basis of 9 0 apfu, is (Ba1.92Pb0.05Sr0.02Na0.01)Sigma(2.00)(Fe0.523+Mn0.293+Al0.15Mg0.06)(Sigma 1.02)(AS(0.64)V(0.36))(Sigma 1.00)O-4](2) [(OH0.92F0.01)(H2O)(0.07)] and the ideal formula is Ba2Fe3+(AsO4)(2)(OH). The crystal structure was solved by direct methods and found to he isostructural to that of arsenbrackebuschite. The structure model was refined (R-1 = 2.6%) on the basis of 1245 observed reflections. Canosioite is named after the small municipality of Canosio, where the type locality, the Valletta mine, is situated. The new mineral and name were approved by the International Mineralogical Association Commission on New Minerals and Mineral Names (IMA2015-030).
机译:新的矿物质夹层,理想的是Ba2Fe3 +(ASO4)(2)(哦)已被发现在Valletta矿,Maim Valley,Capeo Province,Piedmont,意大利。其起源可能与矿石和水热流体之间的反应有关。它发生在红褐色颗粒,次赤毫米尺寸的晶体中,具有淡黄色条纹和玻璃体光泽。甘露糖苷与AegiNe,Baryte,方解石,赤铁矿,青铜Mn含量,未识别的Mn氧化物和未识别的砷化物有关。甘露黄酸盐是双轴(+),带有= 84(2)℃。X =棕黄色,Y =棕色,Z =红棕色Z> Y> X甘露糖是单斜硅,P21 / m,带有= 7.8642 (4),H = 6.1083(3),C = 9.1670(5)埃,β= 112.874(6)度,V = 405.73(4)埃埃(3)和Z = 2.计算密度为4.943g cm(3 )。观察到的粉末X射线衍射图案的七条最强的衍射线是[D是否在肚子中,(I)(HKI)):3.713(18)(111),3.304(100)(21(1)(21(1)),3.058 (31)(020),3.047(59)(103),2.801(73)(112),2.337(24)(220),2.158(24)(123)。电子微探针分析(重量%):Na2O 0.06,MgO 0.43,CaO 0.02,NiO 0.02,CuO 0.03,SrO 0.42,BaO 49.36,PHO 1.69,Al2O3 1.25,Mn2O3 3.89,Fe2O3 6.95,Sb2O3 0.01,SiO2 0.03,P2O5 0.02,V2O5 10.88,AS2O5 24.64,SO 3 0.01,F 0.02,H2O 1.61根据每种配方单元1(OH,F,H2O)组计算。红外光谱证实了OK的存在在9 0 APFU的基础上计算的经验公式,是(Ba1.92pb0.05sr0.02na0.01)sigma(2.00)(Fe0.523 + Mn0.293 + Al0.15mg0.06) (Sigma 1.02)(AS(0.64)V(0.36))(Sigma 1.00)O-4](2)[(OH0.92F0.01)(H2O)(0.07)],理想的公式是Ba2Fe3 +(ASO4)( 2)(哦)。通过直接方法解决晶体结构,并发现他对阿森布克斯布斯基岩的isosoStronation。基于1245个观察的反射,结构模型被精制(R-1 = 2.6%)。甘蔗渣以Canosio的小型城市命名,其中型地方,瓦莱塔矿,位于瓦莱塔矿。新的矿产和名称批准了国际矿物学协会委员会新矿产和矿物名称(IMA2015-030)。

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