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ブータン中部プナカにおける埋没腐植土の ^<14>C年代(タンデトロン加速器質量分析計業績報告2004(平成16)年度)
https://doi.org/10.18999/sumrua.16.144
https://doi.org/10.18999/sumrua.16.14449ec47c2-7fa2-4547-9715-0e54ae445a2f
名前 / ファイル | ライセンス | アクション |
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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公開日 | 2010-06-07 | |||||
タイトル | ||||||
タイトル | ブータン中部プナカにおける埋没腐植土の ^<14>C年代(タンデトロン加速器質量分析計業績報告2004(平成16)年度) | |||||
その他のタイトル | ||||||
その他のタイトル | ^<14>C age of the buried soil in the Punakha area, Bhutan(Summaries of Researches Using AMS) | |||||
著者 |
桧垣, 大助
× 桧垣, 大助× HIGAKI, Daisuke× 上田, 豊× AGETA, Yutaka× 梅村, 順× UMEMURA, Jun× 伏見, 硯二× FUSHIMI, Hiroji |
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権利 | ||||||
権利情報 | 名古屋大学年代測定資料研究センター | |||||
権利 | ||||||
権利情報 | 本文データは学協会の許諾に基づきCiNiiから複製したものである | |||||
抄録 | ||||||
内容記述 | ^<14>C dating of the buried humic soil was carried out to know the age of large-scale GLOF occurrence along the Tsang Chhu River in the Punakha area in Bhutan. Top layer of the buried soil was dated 2,924+28 (1σ) y.B.R(NUTA2-7773). It is younger than the expected age of the Bajo terrace surface, which was formed before the M2 terrace along the Tsang Chhu River in the Last Glacial Period. The reason of it might be that the humic soil was formed on the alluvial fan deposits overlain by the moved mass of the sandy deposits of the Bajo terrace. | |||||
内容記述タイプ | Abstract | |||||
内容記述 | ||||||
内容記述 | タンデトロン加速器質量分析計業績報告 Summaries of Researches Using AMS 2004 (平成16)年度 | |||||
内容記述タイプ | Other | |||||
出版者 | ||||||
出版者 | 名古屋大学年代測定資料研究センター | |||||
言語 | ||||||
言語 | jpn | |||||
資源タイプ | ||||||
資源 | http://purl.org/coar/resource_type/c_6501 | |||||
タイプ | departmental bulletin paper | |||||
ID登録 | ||||||
ID登録 | 10.18999/sumrua.16.144 | |||||
ID登録タイプ | JaLC | |||||
関連情報 | ||||||
関連タイプ | isVersionOf | |||||
識別子タイプ | URI | |||||
関連識別子 | http://ci.nii.ac.jp/naid/110007150921/ | |||||
書誌情報 |
名古屋大学加速器質量分析計業績報告書 巻 16, p. 144-147, 発行日 2005-03 |
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フォーマット | ||||||
application/pdf | ||||||
著者版フラグ | ||||||
値 | publisher |