astro.wikisort.org - MeteoriteThe Yamato 691 (abbreviated Y-691) is the 4.5 billion year old chondrite meteorite discovered by members of the Japanese Antarctic Research Expedition[3] on the blue ice field of the Queen Fabiola Mountains (Yamato Mountains) in Antarctica, on December 21, 1969.[2]
| Yamato 691 |
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| Type | Chondrite |
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| Class | Enstatite chondrite |
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| Composition | Pl(An32-75), En99.2Wo-0.3, tro., nini., oldh., perr., schr., metal(2.2-2.5%Ni, 0.16-0.22%Co)[1] |
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| Country | Antarctica |
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| Region | Queen Fabiola Mountains (Yamato Mountains) |
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| Coordinates | 71°50′S 36°15′E[2] |
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| Observed fall | No |
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| Fall date | 4.5 billion years ago |
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| Found date | December 21, 1969 |
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| TKW | 715 grams (1.576 lb) |
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History
Yamato 691 was one among 9 meteorite specimens identified by the Japanese Expedition Team in 1969. It was later studied at the Max Planck Institute for Chemistry, Mainz, Germany.[4]
In April 2011, NASA and co-researchers from the United States, South Korea and Japan have found a new mineral named "Wassonite" in Yamato 691.[5]
Composition and classification
This meteorite is a stony enstatite chondrite. Minerals reported from the meteorite include:[6]
- Troilite
- Spinel
- Augite
- Diopside
- Enstatite
- Pigeonite
- Albite
- Nepheline
- Iron
- Olivine
- Wassonite - discovered in April, 2011
See also
References
External links
Meteorites and meteoritics |
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| Classification | By type, class, clan, group and grouplet | | Chondrite |
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| Achondrite | | Primitive | |
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| Stony-iron | |
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| Structural |
- Ataxite
- Hexahedrite
- Octahedrite
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| Obsolete terms | |
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Mineralogy and petrology |
- Characteristics
- Grains
- Minerals
- Ca–Al-rich inclusion
- extraterrestrial materials
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- Patterns
- Neumann lines
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- CI1 fossils
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На других языках
- [en] Yamato 691
[ru] Ямато 691
Ямато 691 (англ. Yamato 691) — метеорит, обнаружен в 1969 году в Антарктике.
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