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変形前のマーカー楕円の性質 ―沖縄島国頭層群嘉陽層の場合―
http://hdl.handle.net/20.500.12000/2992
http://hdl.handle.net/20.500.12000/2992bc6fda5b-82a5-4368-9b7d-ae7dc9ee467c
名前 / ファイル | ライセンス | アクション |
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Item type | デフォルトアイテムタイプ(フル)(1) | |||||||||
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公開日 | 2008-01-17 | |||||||||
タイトル | ||||||||||
タイトル | 変形前のマーカー楕円の性質 ―沖縄島国頭層群嘉陽層の場合― | |||||||||
言語 | ja | |||||||||
タイトル | ||||||||||
タイトル | Properties on the initial marker ellipses ―in the case of the Kayo Formation, Kunchan Group, Okinawa-jima― | |||||||||
言語 | en | |||||||||
作成者 |
林, 大五郎
× 林, 大五郎
× Hayashi, Daigoro
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アクセス権 | ||||||||||
アクセス権 | open access | |||||||||
アクセス権URI | http://purl.org/coar/access_right/c_abf2 | |||||||||
主題 | ||||||||||
言語 | en | |||||||||
主題Scheme | Other | |||||||||
主題 | marker ellipse | |||||||||
主題 | ||||||||||
言語 | en | |||||||||
主題Scheme | Other | |||||||||
主題 | finite strain analysis | |||||||||
主題 | ||||||||||
言語 | en | |||||||||
主題Scheme | Other | |||||||||
主題 | initial fabric | |||||||||
主題 | ||||||||||
言語 | en | |||||||||
主題Scheme | Other | |||||||||
主題 | Kayo Formation | |||||||||
主題 | ||||||||||
言語 | en | |||||||||
主題Scheme | Other | |||||||||
主題 | Kunchan Group | |||||||||
主題 | ||||||||||
言語 | en | |||||||||
主題Scheme | Other | |||||||||
主題 | Okinawa-jima | |||||||||
内容記述 | ||||||||||
内容記述タイプ | Other | |||||||||
内容記述 | The method that estimates the initial marker ellipse and the averaged initial ellipse is described. Finite strain analysis carried out previously on the Kayo Formation, Kunchan Group, Okinawa-jima (Hayashi, 1988, 1989) is again examined. It is considered that most of the quartz grain markers do not have initial fabrics from the observation of the distribution tendency of long axes of initial marker ellipses. This is also confirmed by the examination with Lisle's symmetric index test and θcurve test (Lisle, 1977, 1985). The strain analysis was performed precisely because the axial ratios of the average initial ellipse are close to 1.O. | |||||||||
内容記述 | ||||||||||
内容記述タイプ | Other | |||||||||
内容記述 | 初期マーカー楕円と平均初期楕円を計算する方法を解説し,沖縄島国頭層群嘉陽層の歪解析(林,1988,1989)を吟味した.初期マーカー楕円の長軸方位の分布から,解析に使用した石英粒子マーカーには初期ファブリックがなかったと考えられる.このことは,Lisle(1977,1985)の対称性指数とθ曲線テストによる検討から確認された.平均初期楕円の軸比が1に近いため歪解析の精度は高いと思われる. | |||||||||
内容記述 | ||||||||||
内容記述タイプ | Other | |||||||||
内容記述 | 論文 | |||||||||
出版者 | ||||||||||
言語 | ja | |||||||||
出版者 | 日本地質学会 | |||||||||
言語 | ||||||||||
言語 | jpn | |||||||||
資源タイプ | ||||||||||
資源タイプ | journal article | |||||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||||||
出版タイプ | ||||||||||
出版タイプ | VoR | |||||||||
出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 | |||||||||
識別子 | ||||||||||
識別子 | http://hdl.handle.net/20.500.12000/2992 | |||||||||
識別子タイプ | HDL | |||||||||
収録物識別子 | ||||||||||
収録物識別子タイプ | ISSN | |||||||||
収録物識別子 | 0016-7630 | |||||||||
収録物識別子 | ||||||||||
収録物識別子タイプ | NCID | |||||||||
収録物識別子 | AN00141768 | |||||||||
収録物名 | ||||||||||
言語 | ja | |||||||||
収録物名 | 地質学雑誌 | |||||||||
書誌情報 |
巻 98, 号 9, p. 841-854 |