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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. 10

北八甲田火山群における最近5000年間の噴火史

https://doi.org/10.18999/sumrua.10.218
https://doi.org/10.18999/sumrua.10.218
d95f4cd0-7765-434d-adf5-8209947b7f2f
名前 / ファイル ライセンス アクション
KJ00000187305.pdf KJ00000187305.pdf (1.2 MB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2010-05-26
タイトル
タイトル 北八甲田火山群における最近5000年間の噴火史
その他のタイトル
その他のタイトル Eruptive history of Kita-Hakkoda volcano group in Japan during the past 5000 years
著者 工藤, 崇

× 工藤, 崇

WEKO 80886

工藤, 崇

Search repository
Kudo, Takashi

× Kudo, Takashi

WEKO 80887

Kudo, Takashi

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奥野, 充

× 奥野, 充

WEKO 80888

奥野, 充

Search repository
Okuno, Mitsuru

× Okuno, Mitsuru

WEKO 80889

Okuno, Mitsuru

Search repository
中村, 俊夫

× 中村, 俊夫

WEKO 80890

中村, 俊夫

Search repository
Nakamura, Toshio

× Nakamura, Toshio

WEKO 80891

Nakamura, Toshio

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 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 eruptive history of Kita-Hakkoda volcano group in the northeast Japan arc during the past 5000 years has been determined by tephra-stratigraphy and AMS ^<14>C dating. Kita-Hakkoda volcano group comprises eleven small-scale stratovolcanoes. We identified seven tephra layers (Hk-J1,Hk-J2,Hk-J3,Hk-1,Hk-2,Hk-3 and Hk-4 in descending order) erupted from this volcano group. The Hk-J1,Hk-J2,and Hk-J3 tephras were erupted from Jigokunuma Pond (100m in diameter) situated on the southwesterm foot of Odake volcano. The distributions of these tephras are limited the area within 300 m from the vent. These tephras were derived from phreatic eruptions. The magnitude of each eruption is less than 10^4 m^3 in volume. Judging from stratigraphic relation with the Towada-a tephra (AD 915), the eruption age of Hk-J1,Hk-J2 and Hk-J3 is estimated to be 500-400 years ago. The Hk-1,Hk-3 and Hk-4 tephras were erupted from the summit crater of Odake volcano. The source vent of the Hk-2 tephra may be Odake or ldodake volcano. The distribution of each tephra is restricted in 4-7 km from the vents. These tephras were derived from phreatic or vulcanian eruptions. The volume of these tephras ranges from 10^6 to 10^5 m^3. On the basis of radiocarbon dates, their ages are estimated to be 2.1 kyr BP for Hk-1,3.0 kyr BP for Hk-2,3.8 kyr BP for Hk-3 and 4.2 kyr BP for
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 1998 (平成10)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 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.10.218
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/110000475606/
書誌情報 名古屋大学加速器質量分析計業績報告書

巻 10, p. 218-234, 発行日 1999-03
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著者版フラグ
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