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Seismic Velocity Structure along the Western Segment of the North Anatolian Fault Zone Imaged by Seismic Tomography
https://doi.org/10.15083/0000032476
https://doi.org/10.15083/000003247684063e8d-424b-4136-a34e-10b8ddadcef2
名前 / ファイル | ライセンス | アクション |
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IHO82302.pdf (1.22MB)
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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公開日 | 2008-03-28 | |||||
タイトル | ||||||
タイトル | Seismic Velocity Structure along the Western Segment of the North Anatolian Fault Zone Imaged by Seismic Tomography | |||||
言語 | en | |||||
言語 | ||||||
言語 | eng | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Seismic tomography | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Poisson's ratio | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | P wave velocity | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Swave velocity | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | North Anatolian Fault zone | |||||
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 | 10.15083/0000032476 | |||||
ID登録タイプ | JaLC | |||||
その他のタイトル | ||||||
その他のタイトル | 地震波トモグラフィによって明らかになった北アナトリア断層西側セグメントの地震波速度構造 | |||||
著者 |
Mohamed, K. Salah
× Mohamed, K. Salah× S., Sahin and M. Kaplan |
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著者別名 | ||||||
識別子Scheme | WEKO | |||||
識別子 | 124128 | |||||
姓名 | モハメド サラー・S. | |||||
著者別名 | ||||||
識別子Scheme | WEKO | |||||
識別子 | 124129 | |||||
姓名 | サヒン・M., カプラン | |||||
著者所属 | ||||||
値 | Earthquake Research Institute, University of Tokyo, Tokyo 113-0032, Japan | |||||
著者所属 | ||||||
値 | Faculty of Engineering and Architecture, Suleyman Demirel University, Isparta, Turkey | |||||
著者所属 | ||||||
値 | General Directorate of Disaster Affairs, Earthquake Research Department, Ankara, Turkey | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | The three-dimensional P and S wave velocity structures of the crust of the central and western segments of the North Anatolian Fault Zone are determined by applying a tomography method to arrival times data generated by local earthquakes that occurred beneath the study area. From the obtained P and S wave velocity models, we further calculate Poisson’s ratio for a more reliable interpretation of the imaged seismic anomalies. With the exception of high-velocity anomalies detected at a depth of 8km, prominent low-velocity zones are clearly visible along most parts of the studied segment down to a depth of 25km. High Poisson’s ratio anomalies are widely distributed in most parts of the studied region. Seismic activity is more intense in the high-velocity and high Poisson’s ratio zones, although it sometimes occurs in low-velocity areas. Large crustal earthquakes occur in areas characterized by a highly heterogeneous velocity structure, but with distinctly high Poisson’s ratio anomalies. These results indicate that the active tectonics of this area are reflected in the seismic velocity structure, and that large crustal earthquakes occur generally in highly heterogeneous zones revealed by seismic tomography. These inferences are of great significance for understanding earthquake-generating processes in areas having intense seismic and tectonic activities such as the Anatolian plate. | |||||
書誌情報 |
Bulletin of the Earthquake Research Institute 巻 82, 号 3, p. 209-223, 発行日 2007 |
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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Scheme | NDC | |||||
主題 | 051.1 | |||||
出版者 | ||||||
出版者 | 地震研究所 | |||||
出版者別名 | ||||||
値 | Earthquake Research Institute, University of Tokyo |