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4. Crustal Structure from Travel Times of Reflected and Refracted Seismic Waves recorded at Wakayama Micro-earthquake Observatory and its Substations
https://doi.org/10.15083/0000033259
https://doi.org/10.15083/00000332591c44a264-095c-420b-977a-88363fdb82bc
名前 / ファイル | ライセンス | アクション |
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ji0491004.pdf (1.6 MB)
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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公開日 | 2008-05-30 | |||||
タイトル | ||||||
タイトル | 4. Crustal Structure from Travel Times of Reflected and Refracted Seismic Waves recorded at Wakayama Micro-earthquake Observatory and its Substations | |||||
言語 | en | |||||
言語 | ||||||
言語 | eng | |||||
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 | 10.15083/0000033259 | |||||
ID登録タイプ | JaLC | |||||
その他のタイトル | ||||||
その他のタイトル | 4.和歌山微小地震観測所およびその衛星観測点て観測された地震反射波および屈折波の走時と地殻構造 | |||||
著者 |
Mizoue, Megumi
× Mizoue, Megumi |
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著者別名 | ||||||
識別子Scheme | WEKO | |||||
識別子 | 129852 | |||||
姓名 | 溝上, 恵 | |||||
著者所属 | ||||||
値 | Earthquake Research Institute | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | Travel time analysis is made for deep crustal reflections in the Kii Peninsula on the basis of the observational data detected at Wakayama Micro-earthquake Observatory, E.R.I. (Earthquake Research Institute). Time distance data of direct and refracted waves are correlated with the data of reflections to evaluate seismic wave velocities in the earth's crust. An interpretation of the time distance data is represented for the reflections from the Conrad and the Mohorovicic discontinuities. The depth of the Conrad discontinuity can be measured as 20-24 km in the western part of the Kii Peninsula with a possible inclination dipping to the west. The depth of the Mohorovicic discontinuity can be estimated as about 30km in the inland area of the Kii Peninsula. Seismic wave velocities in the upper and the lower crustal layers are estimated as 5.80 km/sec and 6.80 km/sec for the P-waves and 3.46km/sec and 4.05 km/sec for the S-waves respectively. The velocities of the Pg and Pn waves are determined as 5.8 km/sec and 7.9 km/sec respectively from the network observations at the observatory.|和歌山微小地震観測所の定常観測資料にもとづいて地殻内部の不連続面での反射波および屈折波の走時解析を行ない紀伊半島の地殻構造との関係を調べた.以下その結果を要約する. | |||||
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 49, 号 1-3, p. 33-62, 発行日 1971-09-30 |
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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 | 453 | |||||
出版者 | ||||||
出版者 | 東京大学地震研究所 | |||||
出版者別名 | ||||||
値 | Earthquake Research Institute, University of Tokyo |