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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. 13

岐阜県上矢作町で見つかった湖成層中の埋もれ木の<14>^C年代測定

https://doi.org/10.18999/sumrua.13.147
https://doi.org/10.18999/sumrua.13.147
b7f62111-6232-457c-86f6-1242c27512df
名前 / ファイル ライセンス アクション
KJ00000187450.pdf KJ00000187450.pdf (221.5 kB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2010-06-01
タイトル
タイトル 岐阜県上矢作町で見つかった湖成層中の埋もれ木の<14>^C年代測定
その他のタイトル
その他のタイトル <14>^C dating of buried tree trunks found in lake sediments in Kamiyahagi-cho, Gifu Prefecture
著者 池田, 晃子

× 池田, 晃子

WEKO 81322

池田, 晃子

Search repository
Ikeda, Akiko

× Ikeda, Akiko

WEKO 81323

Ikeda, Akiko

Search repository
丹生, 越子

× 丹生, 越子

WEKO 81324

丹生, 越子

Search repository
Niu, Etsuko

× Niu, Etsuko

WEKO 81325

Niu, Etsuko

Search repository
中村, 俊夫

× 中村, 俊夫

WEKO 81326

中村, 俊夫

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Nakamura, Toshio

× Nakamura, Toshio

WEKO 81327

Nakamura, Toshio

Search repository
鈴木, 和博

× 鈴木, 和博

WEKO 81328

鈴木, 和博

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Suzuki, Kazuhiro

× Suzuki, Kazuhiro

WEKO 81329

Suzuki, Kazuhiro

Search repository
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 Umi is located in the Kamiyahagi area of Gifu Prefecture. The name "Umi" means "sea" or "large lake" ; however, there are no large lakes in Gifu, which is an inland prefecture. There is also no information about the origins of the name "Umi" in ancient documents. In September 2000,an enormous storm (called "Tokai Gou-u")occurred in the Tokai Area. Rivers were flooded in the Kamiyahagi area, where embankments and roads near the rivers were destroyed. After the storm many buried trees were exposed on the banks of the Kamimura River, and sedimentary layers typical of a lake setting were found on the both river walls. This was the first evidence for the existence of a palaeo-lake in the area. A geological event such as an earthquake was probably responsible for creating a lake environment, and subsequent lateral degradation of area provided a source for the lake sediments. To determine when this geological event occurred, we measured the ages of tree trunks taken from the lake sediments. Tree trunks that included bark were chosen and samples were taken from the outermost tree rings. After ultrasonic washing, each sample was treated with 1.2N HCl and 1.2N NaOH, rinsed with distilled water to completely remove the acid, and then dried in an oven. Each sample was then sealed in evacuated Vycol tubes with CuO wires and combusted to produce carbon dioxide, water and other trace substances. The carbon dioxide was extracted and purified, and then reduced with powdered iron and hydrogen gas to produced graphite. The graphite was then pressed into target holders and the carbon isotope ratio was measured with the Tandetron Accelerator Mass Spectrometer at Nagoya University. In this study we obtained the ages of tree trunks, which show near the age Tensho earthquake happened. The trees grew shortly before the Tensho earthquake of 1586 A.D., a known large-scale geological event. We consider the Tensho earthquake and its effects to be responsible for the formation of a large lake and the deposition of lake sediments.
内容記述タイプ Abstract
内容記述
内容記述 第14回名古屋大学タンデトロン加速器質量分析計シンポジウム(平成13 (2001)年度)報告
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.13.147
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/110000475726/
書誌情報 名古屋大学加速器質量分析計業績報告書

巻 13, p. 147-150, 発行日 2002-03
フォーマット
application/pdf
著者版フラグ
値 publisher
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