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  1. 131 地震研究所
  2. 東京大学地震研究所彙報
  3. 40
  4. 3
  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. 40
  5. 3

1962年4月30日宮城県北部地震調査報告 : 1900年5月12日陸前北部地震との比較

https://doi.org/10.15083/0000033779
https://doi.org/10.15083/0000033779
858b5035-b617-4c93-a22e-683bc7a5c6b7
名前 / ファイル ライセンス アクション
ji0403013.pdf ji0403013.pdf (881.1 kB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2009-10-13
タイトル
タイトル 1962年4月30日宮城県北部地震調査報告 : 1900年5月12日陸前北部地震との比較
言語 ja
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 10.15083/0000033779
ID登録タイプ JaLC
その他のタイトル
その他のタイトル Studies of the Northern Miyagi Earthquake on April 30th, 1962 : Compared with the Northern Rikuzen Earthquake on May 12th, 1900
著者 音田, 功

× 音田, 功

WEKO 131853

音田, 功

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著者別名
識別子Scheme WEKO
識別子 131854
姓名 Onda, Isao
著者所属
著者所属 地震研究所
抄録
内容記述タイプ Abstract
内容記述 The Northern Miyagi Earthquake on April 30th, 1962 shook almost the same area as the Northern Rikuzen Earthquake on May 12th, 1900 with almost equal intensity The writer compared both earthquakes with one anothor and reached the following conclusions. Magnitude: The magnitude of the 1900 earthquake was larger than that of the later one by about two thirds, deduced by means of Kawasumi's method from the area of the isoseismals. The magnitudes Mk and M in the later one were deduced as 3.6 and 6.6, respectively (Fig. 2). Epicentre: The epicentre of the present one was determined in the neighbourhood of 38°45'N and 141°08'E, from the analysis of the record of the strong motion seismometer at Ishinomaki Weather Station. Therefore, that of the later one was about 20 km distance north from that of the previous one (Fig. 3). It was also ascertained that earthquakes seldom.occur in the northern part of Sendai Plain, although someone doubted its exsitence in that area. Number of after-shocks felt: Twenty-four after shocks were felt up to May 31st in the case of the former earthquake at Ishinomaki, while thirteen up to May 19th in the present earthquake. It was considered that this difference was caused by the dissimilar magnitute and epicentral distance from one another. Many abnormal after-shock were felt at the Hosokura Mine (Table III), compared with those felt at Ishinimaki (Table II) and Tsukidate (Table IV). Characteristics of the earthquake motion: The gravestones at Sekiun Shrine, Matsuyama Town, were studied. There were some gravestones which were rotated counterclockwise in the past earthquake, while such rotations of the gravestones could not be discerned in the case of the present one. It was inferred that this difference resulted from that of the epicentral distance and the magnitude.
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 40, 号 3, p. 613-623, 発行日 1962-11-30
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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