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Magnetic Classification of Stony Meteorites (IV)
https://nipr.repo.nii.ac.jp/records/1061
https://nipr.repo.nii.ac.jp/records/10615f388fb1-ed9a-4cb7-85e5-674b8e06068b
名前 / ファイル | ライセンス | アクション |
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KJ00000011605.pdf (867.8 kB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
---|---|---|---|---|---|---|
公開日 | 1979-12-01 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | Magnetic Classification of Stony Meteorites (IV) | |||||
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) |
Nagata, Takesi
× Nagata, Takesi |
|||||
著者所属(英) | ||||||
en | ||||||
National Institute of Polar Research | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | The intensity of saturation magnetization (I_s) and a ratio of the saturation magnetization of α-phase FeNi component to I_s, I_s (α)/I_s, of 1 E-chondrite, 8 H-chondrites, 10 L-chondrites, 3 LL-chondrites, 8 C-chondrites, 6 diogenites, 1 howardite and 3 eucrites are plotted on an I_s versus I_s (α)/I_s diagram. On this diagram, E-, H-, L-, LL- and C-chondrites and achondrites are well separately grouped to be magnetically identified. | |||||
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 15, p. 273-279, 発行日 1979-12 |