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Natural Quasicrystals
by
Bindi, Luca
, Yao, Nan
, Steinhardt, Paul J
, Lu, Peter J
in
Alloys
/ Aluminum
/ Atomic structure
/ copper
/ Crystal structure
/ Crystallography
/ Crystals
/ Earth sciences
/ Earth, ocean, space
/ Exact sciences and technology
/ Geology
/ Integers
/ iron
/ Mathematical vectors
/ Mineralogy
/ Minerals
/ Mountains
/ Non silicates
/ Rapid quenching
/ Russia
/ Symmetry
/ Tessellations
/ Wave diffraction
2009
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Natural Quasicrystals
by
Bindi, Luca
, Yao, Nan
, Steinhardt, Paul J
, Lu, Peter J
in
Alloys
/ Aluminum
/ Atomic structure
/ copper
/ Crystal structure
/ Crystallography
/ Crystals
/ Earth sciences
/ Earth, ocean, space
/ Exact sciences and technology
/ Geology
/ Integers
/ iron
/ Mathematical vectors
/ Mineralogy
/ Minerals
/ Mountains
/ Non silicates
/ Rapid quenching
/ Russia
/ Symmetry
/ Tessellations
/ Wave diffraction
2009
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Do you wish to request the book?
Natural Quasicrystals
by
Bindi, Luca
, Yao, Nan
, Steinhardt, Paul J
, Lu, Peter J
in
Alloys
/ Aluminum
/ Atomic structure
/ copper
/ Crystal structure
/ Crystallography
/ Crystals
/ Earth sciences
/ Earth, ocean, space
/ Exact sciences and technology
/ Geology
/ Integers
/ iron
/ Mathematical vectors
/ Mineralogy
/ Minerals
/ Mountains
/ Non silicates
/ Rapid quenching
/ Russia
/ Symmetry
/ Tessellations
/ Wave diffraction
2009
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Journal Article
Natural Quasicrystals
2009
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Overview
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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