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Yamato-694 Meteorite: Chemical Composition of Silicate Minerals and Petrographic Nature
https://nipr.repo.nii.ac.jp/records/962
https://nipr.repo.nii.ac.jp/records/962787a138b-4140-44ab-b3a3-af68d691d0ea
名前 / ファイル | ライセンス | アクション |
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KJ00000011508 (690.5 kB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1979-03-01 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | Yamato-694 Meteorite: Chemical Composition of Silicate Minerals and Petrographic Nature | |||||
言語 | ||||||
言語 | eng | |||||
資源タイプ | ||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||
資源タイプ | departmental bulletin paper | |||||
ページ属性 | ||||||
内容記述タイプ | Other | |||||
内容記述 | P(論文) | |||||
著者名(英) |
Okada, Akihiko
× Okada, Akihiko× Shima, Makoto |
|||||
著者所属(英) | ||||||
en | ||||||
The Institute of Physical and Chemical Research | ||||||
著者所属(英) | ||||||
en | ||||||
The Institute of Physical and Chemical Research | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Yamato-694 meteorite collected near the Yamato Mountains in Antarctica in 1969 is an ordinary chondrite belonging to a high-iron group. Major chemical composition of its silicate minerals was determined by electron probe microanalysis. Molar composition of olivine, orthopyroxene and plagioclase is (Fo)_<81>, (En)_<82> and (An)_<10>, respectively. In comparison with the analytical data of silicate minerals in ordinary chondrites, the chemical composition of olivine, orthopyroxene and plagioclase in Yamato-694 meteorite agrees with that of silicate grains in equilibrated high-iron chondrites. The result corresponds to the microscopic feature of this meteorite specimen showing an advanced recrystallization texture. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA00733561 | |||||
書誌情報 |
Memoirs of National Institute of Polar Research. Special issue 巻 12, p. 109-113, 発行日 1979-03 |