首页> 外文期刊>THE CANADIAN MINERALOGIST >STRUCTURAL AND PHYSICAL PROPERTIES OF FISCHESSERITE, A RARE GOLD-SILYER SELENIDE FROM THE DE LAMAR MINE, OWYHEE COUNTY, IDAHO, USA
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STRUCTURAL AND PHYSICAL PROPERTIES OF FISCHESSERITE, A RARE GOLD-SILYER SELENIDE FROM THE DE LAMAR MINE, OWYHEE COUNTY, IDAHO, USA

机译:美国爱达荷州奥威县的拉马斯矿中一种稀有金-锡硒化物-菲泽石的结构和物理性质

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Fischesserite, Ag_3AuSe_2, from the De Lamar mine, Owyhee County, Idaho, USA, was chemically and structurally analyzed. Electron-microprobe analyses give the chemical formula Ag_(2.98)Cu_(0.01)Au_(0.97)Se_(2.03). Fischesserite is optically isotropic, silver white in color with a metallic luster. In reflected light, the mineral is pink. Where observed near naumannite, it appears darker with slightly bluish tints. Reflectivity values are 32.5 (471.1 nm), 30.0 (548.3 nm), 31.1 (586.6 nm), and 33.7 percent (652.3 nm). Fischesserite is cubic, space group 14_132, with a 9.965(1) A, V 989.5(2) A~3 and Z = 8. The crystal structure has been refined to R = 2.69 percent. Fischesserite exhibits a garnet-like structure consisting of edge-sharing Ag[Se_4Ag_2Au_2] and Au[Ag_6Se_2] polyhedra. Fischesserite is confirmed to be isotypic with petzite, Ag_3AuTe_2. The different crystal-chemical environments of noble metals in fischesserite and petzite are compared with those found in other silver-gold chalcogenides.
机译:对来自美国爱达荷州Owyhee县De Lamar矿的Fischesserite Ag_3AuSe_2进行了化学和结构分析。电子探针分析给出化学式Ag_(2.98)Cu_(0.01)Au_(0.97)Se_(2.03)。硅藻土为光学各向同性,银白色,具有金属光泽。在反射光下,矿物质为粉红色。在诺曼石附近观察到的地方,它看起来更暗,略带蓝色。反射率值为32.5(471.1 nm),30.0(548.3 nm),31.1(586.6 nm)和33.7%(652.3 nm)。硅藻土是立方的,空间群14_132,具有9.965(1)A,V 989.5(2)A〜3和Z =8。晶体结构已细化为R = 2.69%。纤锌矿呈现出由边缘共享的Ag [Se_4Ag_2Au_2]和Au [Ag_6Se_2]多面体组成的石榴石状结构。纤锌矿被证实与蓬松石Ag_3AuTe_2是同型的。将纤锌矿和辉石中贵金属的不同晶体化学环境与其他银金硫属化物中发现的晶体化学环境进行了比较。

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