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Icosahedrite, the Glossary

Index Icosahedrite

Icosahedrite is the first known naturally occurring quasicrystal phase.[1]

Table of Contents

  1. 29 relations: Bya, Carbonaceous chondrite, Corundum, Cupalite, Dan Shechtman, Diopside, Dov Levine, Forsterite, Hermann–Mauguin notation, International Mineralogical Association, Khatyrka (river), Khatyrkite, Koryak Mountains, Luca Bindi, Metallurgy, Mineral, Nadia Drake, Nepheline, Nobel Prize in Chemistry, Paul Steinhardt, Phase (matter), Quasicrystal, Serpentinite, Sodalite, Space group, Spinel, Stishovite, Ultramafic rock, University of Florence.

  2. Geology of Russia
  3. Quasicrystals

Bya

bya or b.y.a. is an abbreviation for "billion years ago".

See Icosahedrite and Bya

Carbonaceous chondrite

Carbonaceous chondrites or C chondrites are a class of chondritic meteorites comprising at least 8 known groups and many ungrouped meteorites.

See Icosahedrite and Carbonaceous chondrite

Corundum

Corundum is a crystalline form of aluminium oxide typically containing traces of iron, titanium, vanadium, and chromium. Icosahedrite and Corundum are aluminium minerals.

See Icosahedrite and Corundum

Cupalite

Cupalite is a rare mineral which is mostly composed of copper and aluminium, but might contain up to several percent of zinc or iron; its chemical structure is therefore described by an approximate formula or. Icosahedrite and Cupalite are aluminium minerals, copper minerals, geology of Russia and Native element minerals.

See Icosahedrite and Cupalite

Dan Shechtman

Dan Shechtman (דן שכטמן; born January 24, 1941). Icosahedrite and Dan Shechtman are quasicrystals.

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Diopside

Diopside is a monoclinic pyroxene mineral with composition.

See Icosahedrite and Diopside

Dov Levine

Dov I. Levine (דב לוין, born July 19, 1958) is an American-Israeli physicist, known for his research on quasicrystals, soft condensed matter physics (including granular materials, emulsions, and foams), and statistical mechanics out of equilibrium. Icosahedrite and Dov Levine are quasicrystals.

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Forsterite

Forsterite (Mg2SiO4; commonly abbreviated as Fo; also known as white olivine) is the magnesium-rich end-member of the olivine solid solution series.

See Icosahedrite and Forsterite

Hermann–Mauguin notation

In geometry, Hermann–Mauguin notation is used to represent the symmetry elements in point groups, plane groups and space groups.

See Icosahedrite and Hermann–Mauguin notation

International Mineralogical Association

Founded in 1958, the International Mineralogical Association (IMA) is an international group of 40 national societies.

See Icosahedrite and International Mineralogical Association

Khatyrka (river)

The Khatyrka (Хатырка; Ватыркан) is a river in Chukotka Autonomous Okrug, Russia.

See Icosahedrite and Khatyrka (river)

Khatyrkite

Khatyrkite is a rare mineral which is mostly composed of copper and aluminium, but may contain up to about 15% of zinc or iron. Icosahedrite and Khatyrkite are aluminium minerals, copper minerals, geology of Russia and Native element minerals.

See Icosahedrite and Khatyrkite

Koryak Mountains

The Koryak Mountains or Koryak Highlands are an area of mountain ranges in Far-Eastern Siberia, Russia, located in Chukotka Autonomous Okrug and in Kamchatka Krai, with a small part in Magadan Oblast.

See Icosahedrite and Koryak Mountains

Luca Bindi

Luca Bindi (born 1971) is an Italian geologist.

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Metallurgy is a domain of materials science and engineering that studies the physical and chemical behavior of metallic elements, their inter-metallic compounds, and their mixtures, which are known as alloys.

See Icosahedrite and Metallurgy

Mineral

In geology and mineralogy, a mineral or mineral species is, broadly speaking, a solid substance with a fairly well-defined chemical composition and a specific crystal structure that occurs naturally in pure form.

See Icosahedrite and Mineral

Nadia Drake

Nadia Drake (born July 6, 1980) is an American science journalist and is the interim Physics Editor at Quanta Magazine.

See Icosahedrite and Nadia Drake

Nepheline

Nepheline, also called nephelite, is a rock-forming mineral in the feldspathoid groupa silica-undersaturated aluminosilicate, Na3KAl4Si4O16, that occurs in intrusive and volcanic rocks with low silica, and in their associated pegmatites. Icosahedrite and Nepheline are aluminium minerals.

See Icosahedrite and Nepheline

Nobel Prize in Chemistry

The Nobel Prize in Chemistry (Nobelpriset i kemi) is awarded annually by the Royal Swedish Academy of Sciences to scientists in the various fields of chemistry.

See Icosahedrite and Nobel Prize in Chemistry

Paul Steinhardt

Paul Joseph Steinhardt (born December 25, 1952) is an American theoretical physicist whose principal research is in cosmology and condensed matter physics.

See Icosahedrite and Paul Steinhardt

Phase (matter)

In the physical sciences, a phase is a region of material that is chemically uniform, physically distinct, and (often) mechanically separable.

See Icosahedrite and Phase (matter)

Quasicrystal

A quasiperiodic crystal, or quasicrystal, is a structure that is ordered but not periodic. Icosahedrite and quasicrystal are quasicrystals.

See Icosahedrite and Quasicrystal

Serpentinite

Serpentinite is a metamorphic rock composed predominantly of one or more serpentine group minerals formed by near to complete serpentinization of mafic to ultramafic rocks.

See Icosahedrite and Serpentinite

Sodalite

Sodalite is a tectosilicate mineral with the formula, with royal blue varieties widely used as an ornamental gemstone. Icosahedrite and Sodalite are aluminium minerals.

See Icosahedrite and Sodalite

Space group

In mathematics, physics and chemistry, a space group is the symmetry group of a repeating pattern in space, usually in three dimensions.

See Icosahedrite and Space group

Spinel

Spinel is the magnesium/aluminium member of the larger spinel group of minerals. Icosahedrite and spinel are aluminium minerals.

See Icosahedrite and Spinel

Stishovite

Stishovite is an extremely hard, dense tetragonal form (polymorph) of silicon dioxide.

See Icosahedrite and Stishovite

Ultramafic rock

Ultramafic rocks (also referred to as ultrabasic rocks, although the terms are not wholly equivalent) are igneous and meta-igneous rocks with a very low silica content (less than 45%), generally >18% MgO, high FeO, low potassium, and are composed of usually greater than 90% mafic minerals (dark colored, high magnesium and iron content).

See Icosahedrite and Ultramafic rock

University of Florence

The University of Florence (Italian: Università degli Studi di Firenze) (in acronym UNIFI) is an Italian public research university located in Florence, Italy.

See Icosahedrite and University of Florence

See also

Geology of Russia

Quasicrystals

References

[1] https://en.wikipedia.org/wiki/Icosahedrite