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Paleomagnetism of Stony Meteorites
https://nipr.repo.nii.ac.jp/records/1062
https://nipr.repo.nii.ac.jp/records/10629f2a8503-ef5b-4a8e-ad38-131ce93120de
名前 / ファイル | ライセンス | アクション |
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KJ00000011606.pdf (1.8 MB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||||
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公開日 | 1979-12-01 | |||||||
タイトル | ||||||||
言語 | en | |||||||
タイトル | Paleomagnetism of Stony Meteorites | |||||||
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
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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 paleointensity for a howardite, an ulerite and three diogenites has been determined. By referring to these five values of paleointensity, the paleointensity for 6 achondrites is determined by comparing their NRM with the saturation IRM (Fuller's method). The paleointensity (F_0) for achondrites thus determined is represented by F_0=(0.11±0.02) Oe. The paleointensity for Allende C_3-chondrite is examined from various standpoints. Four other C-chondrites having reasonably stable NRM also are paleomagnetically examined. The average paleointensity for the C-chondrites is F_0=(1.02±0.09) Oe. Ordinary chondrites have a less stable NRM so that the evaluated paleointensity for ordinary chondrites is less reliable. The paleointensity for comparatively stable ordinary chondrites ranges from 0.1 to 0.4 Oe. | |||||||
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. 280-293, 発行日 1979-12 |