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宝飯郡一宮町の豊川河床より産出する大型カキ化石の絶対年代
https://doi.org/10.18999/sumrua.2.62
https://doi.org/10.18999/sumrua.2.6213d92460-38b0-40c7-bdbd-f13dd0fb4fba
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 | 2010-04-23 | |||||
タイトル | ||||||
タイトル | 宝飯郡一宮町の豊川河床より産出する大型カキ化石の絶対年代 | |||||
その他のタイトル | ||||||
その他のタイトル | Radiocarbon Age of the Large-sized Oysters from the Bottom of the Toyo River, Ichinomiya-cho, Hoi-gun | |||||
著者 |
中尾, 宜民
× 中尾, 宜民× Nakao, Yoshitami× 森, 忍× Mori, Shinobu× 池田, 芳雄× Ikeda, Yoshio |
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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 | The mud which is marine in origin is known to be present along the bottom of the Toyo River, Ichinomiya-cho, Hoi-gun. The radiocarbon age is determined by the large-sized oysters found in this mud on the northern side of the Kanazawa bridge across the Toyo River. The result of ^<14>C measurement reveals that the age of the oysters in 29,630±350y.B.P. This datum is nearly equal to the ^<14>C age of shells found in the Kozakai mud, 26,430±1,010y.B.P. according to IKEDA (1973). Fig. 2 shows the paleogeographical map assuming that the height of the former shoreline was 17m, because the height of the mud on the northern side of the Kanazawa bridge is now 17m. Fig. 2 also supports the idea that the mud exposed along the bottom of the Toyo River, Ichinomiya-cho, is correlative with the Kozakai mud. | |||||
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.2.62 | |||||
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/110000475764/ | |||||
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. 62-63, 発行日 1991-03 |
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フォーマット | ||||||
application/pdf | ||||||
著者版フラグ | ||||||
値 | publisher |