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      Natural quasicrystals.

      1 , , ,
      Science (New York, N.Y.)

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          Abstract

          Quasicrystals are solids whose atomic arrangements have symmetries that are forbidden for periodic crystals, including configurations with fivefold symmetry. All examples identified to date have been synthesized in the laboratory under controlled conditions. Here we present evidence of a naturally occurring icosahedral quasicrystal that includes six distinct fivefold symmetry axes. The mineral, an alloy of aluminum, copper, and iron, occurs as micrometer-sized grains associated with crystalline khatyrkite and cupalite in samples reported to have come from the Koryak Mountains in Russia. The results suggest that quasicrystals can form and remain stable under geologic conditions, although there remain open questions as to how this mineral formed naturally.

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          Most cited references7

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          Elasticity and dislocations in pentagonal and icosahedral quasicrystals.

          (1985)
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            Distortion and Peak Broadening in Quasicrystal Diffraction Patterns

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              Non-commensurate (misfit) layer structures

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                Author and article information

                Journal
                Science
                Science (New York, N.Y.)
                1095-9203
                0036-8075
                Jun 5 2009
                : 324
                : 5932
                Affiliations
                [1 ] Museo di Storia Naturale, Sezione di Mineralogia, Università degli Studi di Firenze, Firenze I-50121, Italy.
                Article
                324/5932/1306
                10.1126/science.1170827
                19498165
                468e1fa5-5978-4a56-9f4e-a8ffc557f39b
                History

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