Structural and physical properties of fischesserite, a rare gold-silver selenide from the de Lamar Mine, Owyhee County, Idaho, USA

被引:25
作者
Bindi, L [1 ]
Cipriani, C [1 ]
机构
[1] Univ Florence, Museo Storia Nat, Sez Mineral & Litol, I-50121 Florence, Italy
关键词
fischesserite; Ag-Au chalcogenides; chemical composition; physical properties; crystal- structure refinement; De Lamar mine; Owyhee County; Icaho;
D O I
10.2113/gscanmin.42.6.1733
中图分类号
P57 [矿物学];
学科分类号
070901 ;
摘要
Fischesserite, Ag3AuSe2, from the De Lamar mine, Owyhee County, Idaho, USA, was chemically and structurally analyzed. Electron-microprobe analyses give the chemical formula Ag2.98Cu0.01Au0.97Se2.03. 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 am), 31.1 (586.6 nm), and 33.7% (652.3 nm). Fischesserite is cubic. space group I4(1)32, with a 9.965(1) Angstrom, V 989.5(2) Angstrom(3) and Z = 8. The crystal structure has been refined to R = 2.69%. Fischesserite exhibits a garnet-like structure consisting of edge-sharing Ag[Se4Ag2Au2] and Au[Ag6Se2] polyhedra. Fischesserite is confirmed to be isotopic with petzite, Ag3AuTe2. The different crystal-chemical environments of noble metals in fischesserite and petzite are compared with those found in other silver-gold chalcogenides.
引用
收藏
页码:1733 / 1737
页数:5
相关论文
共 20 条
[1]  
Barton MD, 1978, CAN MINERAL, V16, P651
[2]  
Bindi L, 2004, AM MINERAL, V89, P1505
[3]  
Bindi L, 2004, AM MINERAL, V89, P1043
[4]  
BOCHEK L.I., 1984, ZAPISKI VSESOYUZNOGO, V113, P356
[5]  
Chamid S, 1978, SOV PHYS-CRYSTALLOGR, V23, P267
[6]  
DOWNS RT, 1993, AM MINERAL, V78, P1104
[7]  
FRUEH AJ, 1959, AM MINERAL, V44, P693
[8]  
Ibers J.A., 1974, INT TABLES XRAY CRYS, VIV
[9]  
JOHAN Z, 1971, B SOC FR MINERAL CR, V94, P381
[10]  
NESTERENKO GV, 1984, ZAP VMO, V113, P602