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IMA 2010-042 = icosahedrite
Posted by Marco E. Ciriotti
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IMA 2010-042 = icosahedrite May 05, 2011 07:26PM |
Registered: 7 years ago Posts: 4,441 |
Reference:
▪ Bindi, L., Steinhardt, P.J., Yao, N., Lu, P.J. (2011): Icosahedrite, Al63Cu24Fe13, the first natural quasicrystal. American Mineralogist, 96, 928-931.
Abstract:
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 µm across, closely associated with spinel, 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 (Rmin = Rmax) 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 a6D = 12.64 Å, with probable space group Fm-3-5. The four strongest X-ray powder-diffraction lines [d in Å (I/I0) (n1,n2,n3,n4,n5,n6)] are: 2.006 (100) (40 042), 2.108 (90) (42 22), 1.238 (30) (60 064), and 3.41 (25) (31 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).
▪ Bindi, L., Steinhardt, P.J., Yao, N., Lu, P.J. (2011): Icosahedrite, Al63Cu24Fe13, the first natural quasicrystal. American Mineralogist, 96, 928-931.
Abstract:
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 µm across, closely associated with spinel, 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 (Rmin = Rmax) 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 a6D = 12.64 Å, with probable space group Fm-3-5. The four strongest X-ray powder-diffraction lines [d in Å (I/I0) (n1,n2,n3,n4,n5,n6)] are: 2.006 (100) (40 042), 2.108 (90) (42 22), 1.238 (30) (60 064), and 3.41 (25) (31 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).
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Re: IMA 2010-042 = icosahedrite October 05, 2011 02:45PM |
Registered: 7 years ago Posts: 166 |
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Re: IMA 2010-042 = icosahedrite January 04, 2012 09:28AM |
Registered: 7 years ago Posts: 4,441 |
New Scientist: [www.newscientist.com]
Scientific American: [www.scientificamerican.com]
Live Science: [www.livescience.com]
BBC: [www.bbc.co.uk]
Nature: [www.nature.com]
The Guardian: [www.guardian.co.uk]
Space.com: [www.space.com]
Dvice: [dvice.com]
Space Daily: [www.spacedaily.com]
Le Scienze: [www.lescienze.it]
La Repubblica: [firenze.repubblica.it]
La Nazione: [www.lanazione.it]
Reference:
▪ Bindi, L., Eiler, J.M., Guan, Y., Hollister, L.S., MacPherson, G., Steinhardt, P.J., Yao, N. (2012): Evidence for the extraterrestrial origin of a natural quasicrystal. Proceedings of the National Academy of Sciences, 110, (in press).
Abstract:
We present evidence that a rock sample found in the Koryak Mountains in Russia and containing icosahedrite, an icosahedral quasicrystalline phase with composition Al63Cu24Fe13, is part of a meteorite, likely formed in the early solar system about 4.5 Gya. The quasicrystal grains are intergrown with diopside, forsterite, stishovite, and additional metallic phases [khatyrkite (CuAl2), cupalite (CuAl), and β-phase (AlCuFe)]. This assemblage, in turn, is enclosed in a white rind consisting of diopside, hedenbergite, spinel (MgAl2O4), nepheline, and forsterite. Particularly notable is a grain of stishovite (from the interior), a tetragonal polymorph of silica that only occurs at ultrahigh pressures (≥10 Gpa), that contains an inclusion of quasicrystal. An extraterrestrial origin is inferred from secondary ion mass spectrometry 18O∕16O and 17O∕16O measurements of the pyroxene and olivine intergrown with the metal that show them to have isotopic compositions unlike any terrestrial minerals and instead overlap those of anhydrous phases in carbonaceous chondrite meteorites. The spinel from the white rind has an isotopic composition suggesting that it was part of a calciumaluminum-rich inclusion similar to those found in CV3 chondrites. The mechanism that produced this exotic assemblage is not yet understood. The assemblage (metallic copper-aluminum alloy) is extremely reduced, and the close association of aluminum (high temperature refractory lithophile) with copper (low temperature chalcophile) is unexpected. Nevertheless, our evidence indicates that quasicrystals can form naturally under astrophysical conditions and remain stable over cosmic timescales, giving unique insights on their existence in nature and stability.
www.pnas.org/cgi/doi/10.1073/pnas.1111115109
Edited 2 time(s). Last edit at 01/04/2012 10:28AM by Marco E. Ciriotti.
Scientific American: [www.scientificamerican.com]
Live Science: [www.livescience.com]
BBC: [www.bbc.co.uk]
Nature: [www.nature.com]
The Guardian: [www.guardian.co.uk]
Space.com: [www.space.com]
Dvice: [dvice.com]
Space Daily: [www.spacedaily.com]
Le Scienze: [www.lescienze.it]
La Repubblica: [firenze.repubblica.it]
La Nazione: [www.lanazione.it]
Reference:
▪ Bindi, L., Eiler, J.M., Guan, Y., Hollister, L.S., MacPherson, G., Steinhardt, P.J., Yao, N. (2012): Evidence for the extraterrestrial origin of a natural quasicrystal. Proceedings of the National Academy of Sciences, 110, (in press).
Abstract:
We present evidence that a rock sample found in the Koryak Mountains in Russia and containing icosahedrite, an icosahedral quasicrystalline phase with composition Al63Cu24Fe13, is part of a meteorite, likely formed in the early solar system about 4.5 Gya. The quasicrystal grains are intergrown with diopside, forsterite, stishovite, and additional metallic phases [khatyrkite (CuAl2), cupalite (CuAl), and β-phase (AlCuFe)]. This assemblage, in turn, is enclosed in a white rind consisting of diopside, hedenbergite, spinel (MgAl2O4), nepheline, and forsterite. Particularly notable is a grain of stishovite (from the interior), a tetragonal polymorph of silica that only occurs at ultrahigh pressures (≥10 Gpa), that contains an inclusion of quasicrystal. An extraterrestrial origin is inferred from secondary ion mass spectrometry 18O∕16O and 17O∕16O measurements of the pyroxene and olivine intergrown with the metal that show them to have isotopic compositions unlike any terrestrial minerals and instead overlap those of anhydrous phases in carbonaceous chondrite meteorites. The spinel from the white rind has an isotopic composition suggesting that it was part of a calciumaluminum-rich inclusion similar to those found in CV3 chondrites. The mechanism that produced this exotic assemblage is not yet understood. The assemblage (metallic copper-aluminum alloy) is extremely reduced, and the close association of aluminum (high temperature refractory lithophile) with copper (low temperature chalcophile) is unexpected. Nevertheless, our evidence indicates that quasicrystals can form naturally under astrophysical conditions and remain stable over cosmic timescales, giving unique insights on their existence in nature and stability.
www.pnas.org/cgi/doi/10.1073/pnas.1111115109
Edited 2 time(s). Last edit at 01/04/2012 10:28AM by Marco E. Ciriotti.
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Re: IMA 2010-042 = icosahedrite January 05, 2012 08:18PM |
Registered: 1 year ago Posts: 322 |
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Re: IMA 2010-042 = icosahedrite January 05, 2012 08:44PM |
Registered: 7 years ago Posts: 261 |
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Re: IMA 2010-042 = icosahedrite June 10, 2012 03:46PM |
Registered: 7 years ago Posts: 4,441 |
The meteorite which contents icosahedrite was now officially recognized: the name is Khatirka.
[www.lpi.usra.edu]
[www.lpi.usra.edu]
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Re: IMA 2010-042 = icosahedrite August 10, 2012 04:27PM |
Registered: 7 years ago Posts: 4,441 |
Further evidence support the extraterrestrial origin of the first natural quasicrystal
Below the text and some links related to new information on the discovery in nature of the first quasi-crystal.
The article just came out in Reports on Progress in Physics: (http://iopscience.iop.org/0034-4885/75/9/092601)
Science Daily: [www.sciencedaily.com]
Nature: [blogs.nature.com]
NBC News: # [www.msnbc.msn.com]. UCS8oaB3DKQ
Daily News: [www.newsdaily.com]
Phys.Org: # [phys.org]
JCP INAF: [www.media.inaf.it]
UFO-News-Now: [ufo-news-now.blogspot.it]
Edited 1 time(s). Last edit at 08/10/2012 04:31PM by Marco E. Ciriotti.
Below the text and some links related to new information on the discovery in nature of the first quasi-crystal.
The article just came out in Reports on Progress in Physics: (http://iopscience.iop.org/0034-4885/75/9/092601)
Science Daily: [www.sciencedaily.com]
Nature: [blogs.nature.com]
NBC News: # [www.msnbc.msn.com]. UCS8oaB3DKQ
Daily News: [www.newsdaily.com]
Phys.Org: # [phys.org]
JCP INAF: [www.media.inaf.it]
UFO-News-Now: [ufo-news-now.blogspot.it]
Edited 1 time(s). Last edit at 08/10/2012 04:31PM by Marco E. Ciriotti.
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Re: IMA 2010-042 = icosahedrite October 26, 2012 10:34AM |
Registered: 7 years ago Posts: 4,441 |
Referenza:
• Drake, N. (2012): Prospecting for Quasicrystals. Siberian journey nets a mineralogical space oddity. Sciences News, 182, 24 pp.
[www.sciencenews.org]
• Drake, N. (2012): Prospecting for Quasicrystals. Siberian journey nets a mineralogical space oddity. Sciences News, 182, 24 pp.
[www.sciencenews.org]
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Re: IMA 2010-042 = icosahedrite October 27, 2012 09:15PM |
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Registered: 7 years ago Posts: 2,066 |
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