Startseite Quasicrystals at extreme conditions: The role of pressure in stabilizing icosahedral Al63Cu24Fe13 at high temperature
Artikel
Lizenziert
Nicht lizenziert Erfordert eine Authentifizierung

Quasicrystals at extreme conditions: The role of pressure in stabilizing icosahedral Al63Cu24Fe13 at high temperature

  • Vincenzo Stagno EMAIL logo , Luca Bindi , Changyong Park , Sergey Tkachev , Vitali B. Prakapenka , H.-K. Mao , Russell J. Hemley , Paul J. Steinhardt und Yingwei Fei
Veröffentlicht/Copyright: 24. November 2015
Veröffentlichen auch Sie bei De Gruyter Brill

Abstract

Icosahedrite, the first natural quasicrystal with composition Al63Cu24Fe13, was discovered in several grains of the Khatyrka meteorite, a CV3 carbonaceous chondrite. The presence of icosahedrite associated with high-pressure phases like ahrensite and stishovite indicates formation at high pressures and temperatures due to an impact-induced shock. Previous experimental studies on the stability of synthetic icosahedral AlCuFe have either been limited to ambient pressure, for which they indicate incongruent melting at ~1123 K, or limited to room-temperature, for which they indicate structural stability up to about 35 GPa. These data are insufficient to experimentally constrain the formation and stability of icosahedrite under the conditions of high pressure and temperature that formed the Khatyrka meteorite. Here we present the results of room-temperature, high-pressure diamond-anvil cells measurements of the compressional behavior of synthetic icosahedrite up to ~50 GPa. High P-T experiments were also carried out using both laser-heated diamond-anvil cells combined with in situ synchrotron X‑ray diffraction (at ~42 GPa) and multi-anvil apparatus (at 21 GPa) to investigate the structural evolution and crystallization of possible coexisting phases. The results demonstrate that the quasiperiodic order of icosahedrite is retained over the P-T range explored. We find that pressure acts to stabilize the icosahedral symmetry at temperatures much higher than previously reported. Direct solidification of AlCuFe quasicrystals from an unusual Al-Cu-rich melt is possible but it is limited to a narrow temperature range. Alternatively, quasicrystals may form after crystallization through solidsolid reactions of Al-rich phases. In either case, our results show that quasicrystals can preserve their structure even after hypervelocity impacts spanning a broad range of pressures and temperatures.

Received: 2015-5-8
Accepted: 2015-7-10
Published Online: 2015-11-24
Published in Print: 2015-11-1

© 2015 by Walter de Gruyter Berlin/Boston

Artikel in diesem Heft

  1. On understanding the structure and composition of crystals
  2. Stable and metastable silicate liquid immiscibility in ferrobasalts
  3. When was the Earth’s conveyor belt set in motion?
  4. Trace element partitioning into sulfide: How lithophile elements become chalcophile and vice versa
  5. Petrology on Mars
  6. Hf and Nd isotope systematics of early Archean komatiites from surface sampling and ICDP drilling in the Barberton Greenstone Belt, South Africa
  7. Quasicrystals at extreme conditions: The role of pressure in stabilizing icosahedral Al63Cu24Fe13 at high temperature
  8. Tracking the thermal decomposition of plasma-sprayed hydroxylapatite
  9. Experimental constraints on bubble formation and growth during magma ascent: A review
  10. Ankerite grains with dolomite cores: A diffusion chronometer for low- to medium-grade regionally metamorphosed clastic sediments
  11. Crystal structure, high-pressure, and high-temperature behavior of carbonates in the K2Mg(CO3)2–Na2Mg(CO3)2 join
  12. Temperature micro-mapping in oscillatory-zoned chlorite: Application to study of a green-schist facies fault zone in the Pyrenean Axial Zone (Spain)
  13. Micro- and nano-characterization of Zn-clays in nonsulfide supergene ores of southern Peru
  14. Mineralogical characterization of individual growth structures of Mn-nodules with different Ni+Cu content from the central Pacific Ocean
  15. The magma plumbing system of the Emeishan large igneous province and its role in basaltic magma differentiation in a continental setting
  16. Weathering of the Ethiopian volcanic province: A new weathering index to characterize and compare soils
  17. Recommended mineral-melt partition coefficients for FRTEs (Cu), Ga, and Ge during mantle melting
  18. Tetrahedral plot diagram: A geometrical solution for quaternary systems
  19. Investigations on alunogen under Mars-relevant temperature conditions: An example for a single-crystal-to-single-crystal phase transition
  20. Crystallization of calcium oxalate hydrates by interaction of calcite marble with fungus Aspergillus niger
  21. Direct and indirect evidence for free oxygen (O2–) in MO-silicate glasses and melts (M = Mg, Ca, Pb)
  22. Effect of fluid composition on growth rate of monazite in quartzite at 1.0 GPa and 1000 °C
  23. Determination of the full elastic tensor of single crystals using shear wave velocities by Brillouin spectroscopy
  24. Temperature dependence of the velocity-density relation for liquid metals under high pressure: Implications for the Earth’s outer core
  25. Thermal, compositional, and compressional demagnetization of cementite
  26. The MnCO3-II high-pressure polymorph of rhodocrosite
  27. Lanthanide tetrads in normalized rare element patterns of zircon from the Koktokay No. 3 granitic pegmatite, Altay, NW China
  28. Hydrogrossular, Ca3Al2(SiO4)3–x(H4O4)x: An ab initio investigation of its structural and energetic properties
  29. High-pressure synthesis of skiagite-majorite garnet and investigation of its crystal structure
  30. Mineralogical evolution of Fe–Si-rich layers at the olivine-water interface during carbonation reactions
  31. High-pressure spectroscopic study of siderite (FeCO3) with a focus on spin crossover
  32. Exploring the potential of Raman spectroscopy for crystallochemical analyses of complex hydrous silicates: I. Amphiboles
  33. Apexite, NaMg(PO4)·9H2O, a new struvite-type phase with a heteropolyhedral cluster
  34. The mechanism of infiltration of metamorphic fluids recorded by hydration and carbonation of epidote-amphibolite facies metabasaltic sills in the SW Scottish Highlands
  35. The axial ratio of hcp Fe and Fe–Ni–Si alloys to the conditions of Earth’s inner core
  36. Shock-induced mobilization of metal and sulfide in planetesimals: Evidence from the Buck Mountains 005 (L6 S4) dike-bearing chondrite
  37. The accretion and differentiation of Earth under oxidizing conditions
  38. Dislocation microstructures in simple-shear-deformed wadsleyite at transition-zone conditions: Weak-beam dark-field TEM characterization of dislocations on the (010) plane
  39. Chemical composition and crystal structure of merrillite from the Suizhou meteorite
Heruntergeladen am 27.9.2025 von https://www.degruyterbrill.com/document/doi/10.2138/am-2015-5412/html
Button zum nach oben scrollen