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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. 15

阿寺断層系湯ヶ峰断層の古地震活動と^<14>C年代(タンデトロン加速器質量分析計業績報告2003(平成15)年度)

https://doi.org/10.18999/sumrua.15.144
https://doi.org/10.18999/sumrua.15.144
9e79abf5-bd19-40c5-94aa-ad8e71da1de3
名前 / ファイル ライセンス アクション
KJ00005461768.pdf KJ00005461768.pdf (498.9 kB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2010-06-03
タイトル
タイトル 阿寺断層系湯ヶ峰断層の古地震活動と^<14>C年代(タンデトロン加速器質量分析計業績報告2003(平成15)年度)
その他のタイトル
その他のタイトル Paleoseismicity of the Yugamine fault constituting the Atera Fault System(Summaries of Researches Using AMS)
著者 廣内, 大助

× 廣内, 大助

WEKO 81693

廣内, 大助

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HIROUCHI, Daisuke

× HIROUCHI, Daisuke

WEKO 81694

HIROUCHI, Daisuke

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安江, 健一

× 安江, 健一

WEKO 81695

安江, 健一

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YASUE, Ken-ichi

× YASUE, Ken-ichi

WEKO 81696

YASUE, Ken-ichi

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内田, 主税

× 内田, 主税

WEKO 81697

内田, 主税

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UCHIDA, Chikara

× UCHIDA, Chikara

WEKO 81698

UCHIDA, Chikara

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平松, 孝晋

× 平松, 孝晋

WEKO 81699

平松, 孝晋

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HIRAMATSU, Takahiro

× HIRAMATSU, Takahiro

WEKO 81700

HIRAMATSU, Takahiro

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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 The Yugamine fault, 10 km in length is in the north-central part of the Atera fault system. We studied the Late Quaternary activity of the Yugamine fault through the trenching survey. We excavated a trench across the scarplet on the L1 terrace at Obayashi district. Some humic Layers and fluvial gravels are exposed on the trench walls. The Yugamine fault cut through these layers to form a linear depression on its NE side. From the structural evidence along the fault plane and angular unconformity, we recognize at least three faulting events in this trench. Event 1:916±28yr.B.P.〜2871±29yr.B.P. (A.D.1161〜B.C.1125) We can find the angular unconformity between unit 2d and unit 2a on the both walls. This possibly shows that the last event occurred after the deposition of unit 2d (2871±29yr.B.P.) and before the deposition of unit 2a (916±28yr.B.P.). Event 2: 2564±30yr.B.P. 〜4382±32yr.B.P. (B.C.601〜B.C.3019) The F2 fault plane cut a bottom of unit 3a and the uppermost termination of F2 fault plane is covered by a colluvium(unit W) which located middle part of unit 3a. The age of this colluvium(unit W) is constrained to be older than upper part of unit 3a(dated at 2564±30yr.B.P.) , and younger than the upper part of unit 3b (dated at 4382±32yr.B.P.). Event 3: Before 9124±37yr.B.P. (B.C.8269〜) We can reveal at least one faulting event since the deposition of the gravel (Unit 6). The age of the gravel is assumed to be older than the bottom of unit 3b (dated at 9124±37yr.B.P.).
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 2003 (平成15)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.15.144
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/110007150887/
書誌情報 名古屋大学加速器質量分析計業績報告書

巻 15, p. 144-150, 発行日 2004-03
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