Icosahedrite, Al63Cu24Fe13, the first natural quasicrystal

被引:59
作者
Bindi, Luca [1 ,2 ]
Steinhardt, Paul J. [3 ,4 ]
Yao, Nan [5 ]
Lu, Peter J. [6 ,7 ]
机构
[1] Univ Florence, Museo Storia Nat, Sez Mineral, I-50121 Florence, Italy
[2] CNR Ist Geosci & Georisorse, Sez Firenze, I-50121 Florence, Italy
[3] Princeton Univ, Princeton Ctr Theoret Sci, Princeton, NJ 08544 USA
[4] Princeton Univ, Joseph Henry Labs, Dept Phys, Princeton, NJ 08544 USA
[5] Princeton Univ, Princeton Inst Sci & Technol Mat, Princeton, NJ 08544 USA
[6] Harvard Univ, Dept Phys, Cambridge, MA 02138 USA
[7] Harvard Univ, SEAS, Cambridge, MA 02138 USA
基金
美国国家科学基金会;
关键词
Icosahedrite; new mineral; natural quasicrystal; electron-microprobe data; reflectance data; X-ray diffraction data; Khatyrka; Kamchatka; Russia;
D O I
10.2138/am.2011.3758
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Icosahedrite, ideally Al63Cu24Fe13, is a new mineral from the Khatyrka River, southeastern Chukhotka, Russia. It occurs as dark gray-black anhedral to subhedral grains up to 100 mu m across, closely associated with spine!, diopside, forsterite, nepheline, sodalite, corundum, stishovite, khatyrkite, cupalite, and an unnamed phase of composition AlCuFe. Icosahedrite is opaque with a metallic luster, possesses a gray streak, and is brittle with an uneven fracture. The density could not be determined. For quasicrystals, by definition, the structure is not reducible to a single three-dimensional unit cell, so neither cell parameters nor Z can be given. In plane-polarized incident light, icosahedrite exhibits neither bireflectance nor pleochroism. Between crossed polars, it is isotropic. Reflectance percentages (R-min = R-max) for the four standard COM wavelengths are 62.3 (471.1 nm), 60.6 (548.3 nm), 58.1 (586.6 nm), and 56.0 (652.3 nm), respectively. The X-ray powder pattern was indexed on the basis of six integer indices, as conventionally used with quasicrystals, where the lattice parameter (in six-dimensional notation) is measured to be a(6D) = 12.64 angstrom, with probable space group Fm (3) over bar (5) over bar. The four strongest X-ray powder-diffraction lines [d in angstrom (I/I-0)(n(1),n(2),n(3),n(4),n(5),n(6))] are: 2.006 (100) (4 (2) over bar0 042), 2.108 (90) (42 (2) over bar (2) over bar 22), 1.238 (30) (60 (4) over bar 064), and 3.41 (25) (31 (1) over bar (1) over bar 11). Average results of 34 electron-microprobe analyses gave, on the basis of total atoms = 100, the formula Al63.11Cu24.02Fe12.78Si0.03Co0.01Ca0.01Zn0.01Cr0.02Cl0.01. The simplified formula is Al63Cu24Fe13, which requires the mass fractions Al 43.02, Cu 38.60, Fe 18.38, total 100.00 wt%. The new mineral is named for the icosahedral symmetry of its internal atomic structure, as observed in its diffraction pattern. Both the new mineral and mineral name have been approved by the Commission on New Minerals, Nomenclature and Classification, IMA (2010-042).
引用
收藏
页码:928 / 931
页数:4
相关论文
共 14 条
[1]  
[Anonymous], CRYSALIS RED VERS 1
[2]  
Bancel P.A., 1991, Quasicrystals: the state of the art, P17
[3]   Natural Quasicrystals [J].
Bindi, Luca ;
Steinhardt, Paul J. ;
Yao, Nan ;
Lu, Peter J. .
SCIENCE, 2009, 324 (5932) :1306-1309
[4]   Radiolarian stratigraphy and origin of the Mesozoic terranes of the continental framework of the northwestern Pacific (Russia) [J].
Filatova, NI ;
Vishnevskaya, VS .
TECTONOPHYSICS, 1997, 269 (1-2) :131-150
[5]  
Janot C., 1994, Quasicrystals: A Primer
[6]   QUASICRYSTALS - A NEW CLASS OF ORDERED STRUCTURES [J].
LEVINE, D ;
STEINHARDT, PJ .
PHYSICAL REVIEW LETTERS, 1984, 53 (26) :2477-2480
[7]   Identifying and indexing icosahedral quasicrystals from powder diffraction patterns [J].
Lu, PJ ;
Deffeyes, K ;
Steinhardt, PJ ;
Yao, N .
PHYSICAL REVIEW LETTERS, 2001, 87 (27) :275507-1
[8]   Quasicrystal and approximant structures in the Al-Cu-Fe system [J].
Quiquandon, M ;
Quivy, A ;
Devaud, J ;
Faudot, F ;
Lefebvre, S ;
Bessiere, M ;
Calvayrac, Y .
JOURNAL OF PHYSICS-CONDENSED MATTER, 1996, 8 (15) :2487-2512
[9]   Unique six-dimensional structural model for Al-Pd-Mn and Al-Cu-Fe icosahedral phases [J].
Quiquandon, Marianne ;
Gratias, Denis .
PHYSICAL REVIEW B, 2006, 74 (21)
[10]  
Razin L.V., 1985, ZAPISKI VSES MINERAL, V114, P90