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This terrace seems to be correlate with the \"Hiradoko\" terrace (about 120ka) in Japan by its hight. But they say age of this terrace is 23ka because this terrace cut the Malan Loess. So ^\u003c14\u003eC ages of loess dolls at Xiazhufan and Zhaitang (type of the Malan Loess) are dated by Tandetron accelerator mass spectrometer as follows ; Loess doll at Xiazhufan, below 5m from the top of terrace. Sample(bulk) 13130±240y.B.P. NUTA-762 Sample A_1 24130±220y.B.P. NUTA-888 Sample B_1 24450±230y.B.P. NUTA-889 Sample C_1 7150±100y.B.P. NUTA-891 Loess doll at Zhaitang, 1.5〜1.8m to the top of the Malan Terrace. Sample A_2 2480±80y.B.P. NUTA-1093 Sample B_2 2410±80y.B.P. NUTA-1111 Sample C_2 2190±80y.B.P. NUTA-1094 These results have shown ^\u003c14\u003eC ages of loess dolls do not indicate ages of loess formation which include loess dolls. 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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. 3

黄土小僧の"放射性炭素年代"について

https://doi.org/10.18999/sumrua.3.62
https://doi.org/10.18999/sumrua.3.62
63aba37d-be52-492e-bcb8-3362d2fba84e
名前 / ファイル ライセンス アクション
KJ00000187528.pdf KJ00000187528.pdf (225.2 kB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2010-04-27
タイトル
タイトル 黄土小僧の"放射性炭素年代"について
その他のタイトル
その他のタイトル Carbon Fourteen Ages of Loess Dolls at Xiazhufan, Sangdong Peninsula and Zhaitang, Xishan near beijin, China
著者 藤井, 昭二

× 藤井, 昭二

WEKO 79509

藤井, 昭二

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Fujii, Shoji

× Fujii, Shoji

WEKO 79510

Fujii, Shoji

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坂本, 亨

× 坂本, 亨

WEKO 79511

坂本, 亨

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Sakamoto, Toru

× Sakamoto, Toru

WEKO 79512

Sakamoto, Toru

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中村, 俊夫

× 中村, 俊夫

WEKO 79513

中村, 俊夫

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Nakamura, Toshio

× Nakamura, Toshio

WEKO 79514

Nakamura, Toshio

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耿, 秀山

× 耿, 秀山

WEKO 79515

耿, 秀山

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趙, 松齢

× 趙, 松齢

WEKO 79516

趙, 松齢

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于, 洪軍

× 于, 洪軍

WEKO 79517

于, 洪軍

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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 There is very fine marine terrace about 20m a.s.l. along the coast of Xiazhufan, northern coast of Shandong Peninsula. This terrace seems to be correlate with the "Hiradoko" terrace (about 120ka) in Japan by its hight. But they say age of this terrace is 23ka because this terrace cut the Malan Loess. So ^<14>C ages of loess dolls at Xiazhufan and Zhaitang (type of the Malan Loess) are dated by Tandetron accelerator mass spectrometer as follows ; Loess doll at Xiazhufan, below 5m from the top of terrace. Sample(bulk) 13130±240y.B.P. NUTA-762 Sample A_1 24130±220y.B.P. NUTA-888 Sample B_1 24450±230y.B.P. NUTA-889 Sample C_1 7150±100y.B.P. NUTA-891 Loess doll at Zhaitang, 1.5〜1.8m to the top of the Malan Terrace. Sample A_2 2480±80y.B.P. NUTA-1093 Sample B_2 2410±80y.B.P. NUTA-1111 Sample C_2 2190±80y.B.P. NUTA-1094 These results have shown ^<14>C ages of loess dolls do not indicate ages of loess formation which include loess dolls. Also, ages mesured in bulk rocks in unable to understand what does its mean because each picking sample A_1,B_1 and C_1 in the same one sample has each age.
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.3.62
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/110000475793/
書誌情報 名古屋大学加速器質量分析計業績報告書

巻 3, p. 62-66, 発行日 1992-03
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