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本州中部のテクトニクスと1993年の静岡の地震
https://doi.org/10.14945/00000335
https://doi.org/10.14945/00000335710a37c8-5f5d-4362-b158-0519a97dc431
名前 / ファイル | ライセンス | アクション |
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KJ00000102391.pdf (1.5 MB)
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||||
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公開日 | 2008-01-25 | |||||||
タイトル | ||||||||
タイトル | 本州中部のテクトニクスと1993年の静岡の地震 | |||||||
言語 | ||||||||
言語 | jpn | |||||||
キーワード | ||||||||
主題Scheme | Other | |||||||
主題 | earthquake | |||||||
キーワード | ||||||||
主題Scheme | Other | |||||||
主題 | Kusanagi Fault | |||||||
キーワード | ||||||||
主題Scheme | Other | |||||||
主題 | Udo Hills | |||||||
キーワード | ||||||||
主題Scheme | Other | |||||||
主題 | tectonics | |||||||
キーワード | ||||||||
主題Scheme | Other | |||||||
主題 | central Japan | |||||||
資源タイプ | ||||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||||
資源タイプ | departmental bulletin paper | |||||||
ID登録 | ||||||||
ID登録 | 10.14945/00000335 | |||||||
ID登録タイプ | JaLC | |||||||
タイトル(別言語) | ||||||||
その他のタイトル | Earthquakes in Shizuoka in 1993 and tectonics of central Japan | |||||||
著者 |
新妻, 信明
× 新妻, 信明
WEKO
181
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書誌情報 |
静岡大学地球科学研究報告 巻 22, p. 11-22, 発行日 1995-07 |
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出版者 | ||||||||
出版者 | 静岡大学地球科学教室 | |||||||
NDC | ||||||||
主題Scheme | NDC | |||||||
主題 | 453 | |||||||
抄録 | ||||||||
内容記述タイプ | Abstract | |||||||
内容記述 | The Crustal Activity Observatory of Shizuoka University has been carrying out seismological observations since 1979. This report describes the results of the seismological observations since 1990,especially on the earthquakes in Shizuoka on 7-11 August 1993,which had a maximum magnitude of 4.2,and their relation to the tectonics of central Japan. The differences in magnitude (ΔM) between Shizuoka University and the Japan Meteorological Agency for 858 earthquakes with an epicenter less than 200 km from the observatory and with a focal depth shallower than 200 km have been examined, and the systematic differences with the focal azimuths are found. The relation between the magnitude and duration of the earthquakes is determined, based on seismological observations from June to August 1993. The foci of the earthquakes in Shizuoka in August 1993 were located on the Kusanagi Fault, and the changes in the ratios of the maximum amplitudes of P and S waves were observed during the earthquakes. The dislocation along the Kusanagi Fault is tilting the Udo Hills about 10°northwestward, and the rate of uplift of the Udo Hills is 4 mm/yr. The Kusanagi Fault is characterized by the landward boundary of a fore-arc basin along the subductive boundary of the Philippine Sea Plate and gravitational collapse. The seismic activities in central Japan are related to the bending of the zonal stucture and collision of the Izu Arc, caused by the motion of the Philippine Sea Plate. Historically, large earthquakes in Shizuoka, Southwest Japan, the northern Fossa Magna, Niigata, Misaka, the Matsuzaki Uplift Zones, and the Zenisu Ridge have happened closely in a time series. | |||||||
ISSN | ||||||||
収録物識別子タイプ | ISSN | |||||||
収録物識別子 | 03886298 | |||||||
NII論文ID | ||||||||
関連タイプ | isIdenticalTo | |||||||
識別子タイプ | NAID | |||||||
関連識別子 | 110000413365 | |||||||
NII書誌ID | ||||||||
収録物識別子タイプ | NCID | |||||||
収録物識別子 | AN00103190 | |||||||
フォーマット | ||||||||
内容記述タイプ | Other | |||||||
内容記述 | application/pdf | |||||||
著者版フラグ | ||||||||
出版タイプ | VoR | |||||||
出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 |