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  1. F300 宇宙地球環境研究所
  2. F300b 紀要
  3. 名古屋大学加速器質量分析計業績報告書
  4. 2

駿河舟状海盆ピストンコア試料の<14>^C年代

https://doi.org/10.18999/sumrua.2.64
https://doi.org/10.18999/sumrua.2.64
48e3f641-56fe-4e24-be2f-35b43f04dcb1
名前 / ファイル ライセンス アクション
KJ00000187497.pdf KJ00000187497.pdf (261.1 kB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2010-04-23
タイトル
タイトル 駿河舟状海盆ピストンコア試料の<14>^C年代
その他のタイトル
その他のタイトル <14>^C ages of the piston core sediments obtained form Suruga trough
著者 志岐, 常正

× 志岐, 常正

WEKO 79421

志岐, 常正

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Shiki, Tsunemasa

× Shiki, Tsunemasa

WEKO 79422

Shiki, Tsunemasa

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中村, 俊夫

× 中村, 俊夫

WEKO 79423

中村, 俊夫

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Nakamura, Toshio

× Nakamura, Toshio

WEKO 79424

Nakamura, Toshio

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中井, 信之

× 中井, 信之

WEKO 79425

中井, 信之

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Nakai, Nobuyuki

× Nakai, Nobuyuki

WEKO 79426

Nakai, Nobuyuki

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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 天然放射性元素測定小委員会
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 Organic carbon content and ^<14>C age have benn measured for solid organic materials of plant residues in two turbidite layers of a piston core (KT7819-24), and of a chip picked up from a pebble layer in another piston core (KT7819-21), from Suruga Trough, off Central Japan. Results are summarized in Table 1. These results support the idea, 1) proposed in our previous paper (Nakamura et al., 1990) that the plant residues in the turbiditite layers of the core (KT7819-24) were originated by river flood, and mixed with older sediments of shallow sea when the sediment layer was overloaded and falled down forming turbidity currents, 2) that the pebble layer distributed in the axial zone of the Suruga Trough of over 2,000 meters deep is very recent sediments of some kinds of glavity flow, as estimated by Sato (1962) concerning his piston core sediments.
内容記述タイプ Abstract
出版者
出版者 名古屋大学年代測定資料研究センター 天然放射性元素測定小委員会
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.2.64
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/110000475766/
書誌情報 名古屋大学加速器質量分析計業績報告書

巻 2, p. 64-69, 発行日 1991-03
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