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The crystal structure of uytenbogaardtite, Ag3AuS2, and its relationships with gold and silver sulfides-selenides

机译:Uytenbogaardtite,Ag3aus2的晶体结构及其与金和硫化银的关系 - 硒化物

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摘要

The crystal structure of the mineral uytenbogaardtite, a rare silver-gold sulfide, was solved using intensity data collected for a crystal from the type locality, the Comstock lode, Storey County, Nevada (USA). The study revealed that the structure is trigonal, space group R (3) over barc, with cell parameters a = 13.6952(5), c = 17.0912(8) angstrom and V = 2776.1(2) angstrom(3). The refinement of an anisotropic model led to an R index of 0.0140 for 1099 independent reflections. The structure consists of a sub-lattice of sulfur atoms forming a distorted body-centred cubic arrangement. The structure contains distinct tri-atomic linear groups (S-Au-S) and Ag atoms bonded to four S atoms (from four different linear groups) in a distorted tetrahedral arrangement. On the basis of information gained from this characterization, uytenbogaardtite is here definitively proved to be structurally different from petzite, Ag3AuTe2 and fischesserite, Ag3AuSe2. By use of high-quality single-crystal diffraction data, the symmetry of the mineral was found to be trigonal, and not tetragonal as erroneously supposed. A revaluation of the powder diffraction data listed in the scientific literature for uytenbogaardtite according to the structural results obtained here leads to an excellent agreement. Crystal-chemical features of uytenbogaardtite, Au2S, petrovskaite AgAuS, uytenbogaardtite-fischesserite series Ag3Au(S-2-Se-x(x)) and acanthite-naummanite series Ag-2(S-1-Se-x(x)) are compared.
机译:使用来自类型位置的晶体的强度数据,来自类型的岩石,内华达州(USA)的岩石仪(美国)的晶体数据来解决矿物Uytenbogaardtite的矿物质结构。该研究表明,该结构是Trigonal,空间组R(3)上Barc,细胞参数A = 13.6952(5),C = 17.0912(8)埃和V = 2776.1(2)埃(3)。各向异性模型的细化导致R指数为0.0140,对于1099个独立的反射。该结构由形成扭曲的体为立方体布置的硫原子的亚晶格组成。该结构含有不同的三原子线性基团(S-AU-S)和粘合到四个S原子(来自四种不同的线性基团)的Ag原子以扭曲的四面体布置。在从该表征中获得的信息的基础上,Uytenbogaardtite在这里明确证明在结构上不同于Petzite,Ag3aute2和Fischesserite,Ag3ause2。通过使用高质量的单晶衍射数据,发现矿物的对称性是三角形,而不是错误的假设。根据此处获得的结构结果,对Uytenbogaardtite的科学文献中列出的粉末衍射数据的重估导致了很好的一致性。 Uytenbogaardtite,Au2s,Petrovskaite Agaus,Uytenbogaardtite-fischesserite系列Ag3au(S-2-Se-x(x))和acanthite-naummanite系列Ag-2(S-1-Se-x(x))的晶体化学特征比较的。

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