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筑波,栃本において同時のおこなつた多点式観測法による関東および中部地方の微小地震の研究
https://doi.org/10.15083/0000033763
https://doi.org/10.15083/0000033763c517a09c-c41e-4608-9269-87b482484a7b
名前 / ファイル | ライセンス | アクション |
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ji0404016.pdf (598.0 kB)
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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公開日 | 2009-02-18 | |||||
タイトル | ||||||
タイトル | 筑波,栃本において同時のおこなつた多点式観測法による関東および中部地方の微小地震の研究 | |||||
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 | 10.15083/0000033763 | |||||
ID登録タイプ | JaLC | |||||
その他のタイトル | ||||||
その他のタイトル | Simultaneous Operation of Seismometer-array Stations in a Study of Micro-earthquakes in the Kanto and Chubu Region | |||||
著者 |
宮村, 攝三
× 宮村, 攝三× 堀, 実× 安芸, 敬一× 辻浦, 賢× 松本, 英照 |
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著者別名 | ||||||
識別子 | 131804 | |||||
識別子Scheme | WEKO | |||||
姓名 | Miyamura, Setumi | |||||
著者別名 | ||||||
識別子 | 131805 | |||||
識別子Scheme | WEKO | |||||
姓名 | Hori, Minoru | |||||
著者別名 | ||||||
識別子 | 131806 | |||||
識別子Scheme | WEKO | |||||
姓名 | Aki, Keiiti | |||||
著者別名 | ||||||
識別子 | 131807 | |||||
識別子Scheme | WEKO | |||||
姓名 | Tsujimura, Masaru | |||||
著者別名 | ||||||
識別子 | 131808 | |||||
識別子Scheme | WEKO | |||||
姓名 | Matsumoto, Hideteru | |||||
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 | A temporary seismometer-array station such as described by Miyamura et al. (1961) was established at Tochimoto and at Tsukuba to investigate the micro-earthquakes occurring in the Kanto and Chubu region. The principal purposes of the present investigation are 1) to find the accuracy of hypocentre determination by the seismometer-array method, 2) to locate the zones of micro-earthquakes in the Kanto and Chubu region and 3) to learn something about the structure of the crust and upper mantle in this region. The epicentres determined independently by the Tsukuba station and by the Tochimoto station are shown in Fig. 9a and Fig. 9b respectively. It is remarkable that many earthquakes in the Western Kanto and Chubu region occur in the crust, while those in East Kanto occur mostly in the upper mantle. Fig. 10 shows the epicentres of 14 shocks for which both stations could give good determinations of them. There is a systematic divergence between the epicentres determined independently at the two stations. This divergence may be explained if the velocity in the upper mantle increases seaward. | |||||
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 4, p. 885-897, 発行日 1963-03-10 |
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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 | 453 | |||||
主題Scheme | NDC | |||||
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 |