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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. 1
  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. 1

伊那谷断層帯小黒川測線における浅層反射法地震探査 : データ取得と処理

https://doi.org/10.15083/0000032482
7964ec26-6b96-4da7-891c-8f701a759a90
名前 / ファイル ライセンス アクション
IHO82103.pdf IHO82103.pdf (9MB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2008-02-28
タイトル
タイトル 伊那谷断層帯小黒川測線における浅層反射法地震探査 : データ取得と処理
言語 ja
言語
言語 jpn
キーワード
主題 Ina valley fault zone
主題Scheme Other
キーワード
主題 high-resolution seismic reflection profiling
主題Scheme Other
キーワード
主題 subsurface structure
主題Scheme Other
キーワード
主題 boundary fault
主題Scheme Other
キーワード
主題 frontal fault
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 10.15083/0000032482
ID登録タイプ JaLC
その他のタイトル
その他のタイトル High-Resolution Seismic Reflection Survey ""Oguro River Seismic Line"" in the Ina Valley Fault Zone, Central Japan : Data Acquisition and Processing
著者 岡田, 真介

× 岡田, 真介

WEKO 124316

岡田, 真介

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池田, 安隆

× 池田, 安隆

WEKO 124317

池田, 安隆

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小田, 晋

× 小田, 晋

WEKO 124318

小田, 晋

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越後, 智雄

× 越後, 智雄

WEKO 124319

越後, 智雄

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戸田, 茂

× 戸田, 茂

WEKO 124320

戸田, 茂

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鈴木, 規眞

× 鈴木, 規眞

WEKO 124321

鈴木, 規眞

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河合, 陽平

× 河合, 陽平

WEKO 124322

河合, 陽平

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加藤, 一

× 加藤, 一

WEKO 124323

加藤, 一

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佐藤, 比呂志

× 佐藤, 比呂志

WEKO 124324

佐藤, 比呂志

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木村, 治夫

× 木村, 治夫

WEKO 124325

木村, 治夫

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田力, 正好

× 田力, 正好

WEKO 124326

田力, 正好

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石山, 達也

× 石山, 達也

WEKO 124327

石山, 達也

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今泉, 俊文

× 今泉, 俊文

WEKO 124328

今泉, 俊文

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楮原, 京子

× 楮原, 京子

WEKO 124329

楮原, 京子

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松多, 信尚

× 松多, 信尚

WEKO 124330

松多, 信尚

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内田, 拓馬

× 内田, 拓馬

WEKO 124331

内田, 拓馬

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宇野, 知樹

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WEKO 124332

宇野, 知樹

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河村, 知徳

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WEKO 124333

河村, 知徳

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著者別名
識別子
識別子 124334
識別子Scheme WEKO
姓名
姓名 Okada, Shinsuke
著者別名
識別子
識別子 124335
識別子Scheme WEKO
姓名
姓名 Ikeda, Yasutaka
著者別名
識別子
識別子 124336
識別子Scheme WEKO
姓名
姓名 Oda, Shin
著者別名
識別子
識別子 124337
識別子Scheme WEKO
姓名
姓名 Echigo, Tomoo
著者別名
識別子
識別子 124338
識別子Scheme WEKO
姓名
姓名 Toda, Shigeru
著者別名
識別子
識別子 124339
識別子Scheme WEKO
姓名
姓名 Suzuki, Norimasa
著者別名
識別子
識別子 124340
識別子Scheme WEKO
姓名
姓名 Kawai, Youhei
著者別名
識別子
識別子 124341
識別子Scheme WEKO
姓名
姓名 Kato, Hajime
著者別名
識別子
識別子 124342
識別子Scheme WEKO
姓名
姓名 Sato, Hiroshi
著者別名
識別子
識別子 124343
識別子Scheme WEKO
姓名
姓名 Kimura, Haruo
著者別名
識別子
識別子 124344
識別子Scheme WEKO
姓名
姓名 Tajikara, Masayoshi
著者別名
識別子
識別子 124345
識別子Scheme WEKO
姓名
姓名 Ishiyama, Tatsuya
著者別名
識別子
識別子 124346
識別子Scheme WEKO
姓名
姓名 Imaizumi, Toshifumi
著者別名
識別子
識別子 124347
識別子Scheme WEKO
姓名
姓名 Kagohara, Kyoko
著者別名
識別子
識別子 124348
識別子Scheme WEKO
姓名
姓名 Matsuta, Nobuhisa
著者別名
識別子
識別子 124349
識別子Scheme WEKO
姓名
姓名 Uchida, Takuma
著者別名
識別子
識別子 124350
識別子Scheme WEKO
姓名
姓名 Uno, Tomoki
著者別名
識別子
識別子 124351
識別子Scheme WEKO
姓名
姓名 Kawamura, Tomonori
著者所属
著者所属 東京大学大学院理学系研究科
著者所属
著者所属 愛知教育大学
著者所属
著者所属 山梨大学教育人間科学部
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 産業技術総合研究所活断層研究センター
著者所属
著者所属 東北大学大学院理学研究科
著者所属
著者所属 山梨大学大学院医学光学総合教育部
著者所属
著者所属 千葉大学大学院自然科学研究科
抄録
内容記述タイプ Abstract
内容記述 Ina Valley Fault Zone consists mainly of two subparallel fault strands: the boundary fault and the frontal fault. The boundary fault is located at the foot of the Kiso range. The frontal fault is located several kilometers east of the boundary fault. Both faults are thrust faults with high rates of horizontal shortening. To reveal the subsurface structure of and relationship between these two faults, we carried out a high-resolution seismic reflection survey along the Oguro River in the northern Ina Valley. The source used in the survey was a mini-vibrator (T-15000). The source and receiver spacing was 10m, with 240-ch geophones used for recording. The seismic section after careful data processing shows that the boundary fault dips west at a fairly low angle and the frontal fault is likely to converge on the boundary fault at depth. Westward dip of basin-fill sediments becomes steeper with increasing depth, indicating that the basin-fill sediments are syntectonic.
書誌情報 地震研究所彙報

巻 82, 号 1, p. 13-23, 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
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内容記述 application/pdf
日本十進分類法
主題 51.1
主題Scheme NDC
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出版者 地震研究所
出版者別名
Earthquake Research Institute, University of Tokyo
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Ver.1 2021-03-01 16:44:55.575698
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