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  1. 131 地震研究所
  2. 東京大学地震研究所彙報
  3. 44
  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. 44
  5. 4

Electro-Optical Measurement of Horizontal Strains Accumulating in the Swarm Earthquake Area (2)

https://doi.org/10.15083/0000033538
https://doi.org/10.15083/0000033538
858f574a-f1d6-4b15-ba28-5f597b07b27c
名前 / ファイル ライセンス アクション
ji0444015.pdf ji0444015.pdf (1.4 MB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2008-05-30
タイトル
タイトル Electro-Optical Measurement of Horizontal Strains Accumulating in the Swarm Earthquake Area (2)
言語 en
言語
言語 eng
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 10.15083/0000033538
ID登録タイプ JaLC
その他のタイトル
その他のタイトル 群発地震活動に伴う地殻変動の観測(2)
著者 Kasahara, Keichi

× Kasahara, Keichi

WEKO 131010

Kasahara, Keichi

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Okada, Atusi

× Okada, Atusi

WEKO 131011

Okada, Atusi

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Shibano, Mutsuro

× Shibano, Mutsuro

WEKO 131012

Shibano, Mutsuro

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Sasaki, Koici

× Sasaki, Koici

WEKO 131013

Sasaki, Koici

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Matsumoto, Shigeo

× Matsumoto, Shigeo

WEKO 131014

Matsumoto, Shigeo

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著者別名
識別子Scheme WEKO
識別子 131015
姓名 笠原, 慶一
著者別名
識別子Scheme WEKO
識別子 131016
姓名 岡田, 惇
著者別名
識別子Scheme WEKO
識別子 131017
姓名 柴野, 睦郎
著者別名
識別子Scheme WEKO
識別子 131018
姓名 佐々木, 幸一
著者別名
識別子Scheme WEKO
識別子 131019
姓名 松本, 滋夫
抄録
内容記述タイプ Abstract
内容記述 The authors have repeated Geodimeter surveys in the Matsushiro area since October, 1965. Their purpose is the study of accumulation of horizontal strains there at various stages of the seismic activity. The present paper will deal mainly with the strain events observed from March of this year, since the data for the earlier period was reported in the previous paper. Generally speaking, the mode of strain accumulation in the present period does not differ much from that previously observed. That is to say, extension predominated in the NS-direction whereas a considerable amount of contraction was observed in the EW-direction. As for the amount of strain accumulation, however, the present period shows an activity much higher than the previous one. Length of the Sorobeku base-line, for example, increased as much as 35cm during the period March to July inclusive, and another 43cm during the following two months. So that the total extension of this baseline after October, 1965, reached 89cm indicating the average linear strain to be 290×10-6. Strain data thus obtained for the three independent base-lines enable us to study the horizontal deformations as a plane-strain problem. Computed principal axes harmonize very well with the seismic force system there. Strain energy associated with the deformations is roughly estimated to be comparable with the energy released by the seismic activity. It is hard to believe that the earth's crust is deformed elastically to such a high strain rate as above-mentioned. We must naturally take non-elastic deformation into consideration for understanding the present event. A fracture zone that has developed remarkably since last spring is notable from this point of view. According to geologists'reports, the systematically arranged fractures seem to suggest a buried fault of strike-slip type that crosses the Sorobeku base-line obliquely. Actual conditions and characteristics of the presumed fault should be urgently studied by taking all the available data into consideration. The authors constructed supplementary networks in the Wakaho and Nakano areas in order to watch strain accumulation in localities adjacent to the present seismic area. Data from the surveys on these networks are also discussed briefly.
書誌情報 東京大學地震研究所彙報 = Bulletin of the Earthquake Research Institute, University of Tokyo

巻 44, 号 4, p. 1715-1733, 発行日 1967-03-31
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Scheme NDC
主題 453
出版者
出版者 東京大学地震研究所
出版者別名
Earthquake Research Institute, University of Tokyo
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