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  1. 131 地震研究所
  2. 東京大学地震研究所彙報
  3. 82
  4. 4
  1. 0 資料タイプ別
  2. 30 紀要・部局刊行物
  3. 東京大学地震研究所彙報
  4. 82
  5. 4

2007年能登半島地震の震源域陸域の地質

https://doi.org/10.15083/0000032465
e4ffff42-be97-4475-9698-f34a1d620ecb
名前 / ファイル ライセンス アクション
IHO82403.pdf IHO82403.pdf (1.5MB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2008-07-15
タイトル
タイトル 2007年能登半島地震の震源域陸域の地質
言語 ja
言語
言語 jpn
キーワード
主題 The 2007 Noto Hanto Earthquake
主題Scheme Other
キーワード
主題 syn-rifting succession
主題Scheme Other
キーワード
主題 stratigraphy
主題Scheme Other
キーワード
主題 earthquake source fault
主題Scheme Other
キーワード
主題 geologic structure
主題Scheme Other
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 10.15083/0000032465
ID登録タイプ JaLC
著者 冨岡, 伸芳

× 冨岡, 伸芳

WEKO 123953

冨岡, 伸芳

Search repository
佐藤, 比呂志

× 佐藤, 比呂志

WEKO 123954

佐藤, 比呂志

Search repository
著者別名
識別子
識別子 123955
識別子Scheme WEKO
姓名
姓名 Tomioka, Nobuyoshi
著者別名
識別子
識別子 123956
識別子Scheme WEKO
姓名
姓名 Sato, Hiroshi
著者所属
著者所属 株式会社ダイヤコンサルタント
著者所属
著者所属 東京大学地震研究所
著者所属
著者所属 Dia Consultants Co., Ltd,
著者所属
著者所属 Earthquake Research Institute, University of Tokyo
抄録
内容記述タイプ Abstract
内容記述 Stratigraphy and geologic structure in the onshore epicentral area of the 2007 Noto Hanto earthquake was studied to reveal the relationship between the earthquake source fault and geologic structure. The epicentral area is located in the southern part of the Yamato basin rift-system and thick syn-rift succession is exposed on the Noto peninsula. Exposed Paleogene to Miocene rocks overlying the Jurasic granitic rocks are divided in ascending order into Daifukuji, Ohkadoma, Anamizu, Nawamata, Touge, Sekinohama, Maehama Formations, and Kurosaki Andesite. The Dai-fukuji and Okadoma Formations consist of sedimentary rocks deposited at the Paleogene pre-rifting stage. More than 1,400m thick, Oligocene to lower Miocene andesitic volcanic rocks and fluvial sediments (Anamizu, Nawamata and Toge Formations) were deposited, filling half grabens bounded by ENE-WSW- and NS-trending faults. They are syn-rift sediments formed at the rifting and open-ing stage of the Sea of Japan. Middle Miocene shallow marine sedimentary rocks (Sekinohama and Maehama Formations) unconformably cover the syn-rift succession. A major geologic structure was formed by rifting associated with the opening of the Sea of Japan. The source fault of the 2007 Noto Hanto earthquake trending NE to ENE coincides with the fault bounding the Miocene halft graben, and its eastern end corresponds to the NS-trending fault, a probable transfer fault during the rifting stage.
書誌情報 地震研究所彙報

巻 82, 号 4, p. 255-264, 発行日 2007
ISSN
収録物識別子タイプ ISSN
収録物識別子 00408972
書誌レコードID
収録物識別子タイプ NCID
収録物識別子 AN00162258
フォーマット
内容記述タイプ Other
内容記述 application/pdf
日本十進分類法
主題 51.1
主題Scheme NDC
出版者
出版者 地震研究所
出版者別名
Earthquake Research Institute, University of Tokyo
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