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59.Revisions of my ""Notes on the Origins of Earthquakes.""
https://doi.org/10.15083/0000034585
https://doi.org/10.15083/00000345856c5b6837-3ddb-4336-9b39-4d40246d339d
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
ji0154008.pdf (350.1 kB)
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| Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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| 公開日 | 2008-06-06 | |||||
| タイトル | ||||||
| タイトル | 59.Revisions of my ""Notes on the Origins of Earthquakes."" | |||||
| 言語 | en | |||||
| 言語 | ||||||
| 言語 | eng | |||||
| 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 | 10.15083/0000034585 | |||||
| ID登録タイプ | JaLC | |||||
| その他のタイトル | ||||||
| その他のタイトル | 59.發震機構に就いて(訂正) | |||||
| 著者 |
Inouye, Win
× Inouye, Win |
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| 著者別名 | ||||||
| 識別子Scheme | WEKO | |||||
| 識別子 | 134093 | |||||
| 姓名 | 井上, 宇胤 | |||||
| 著者所属 | ||||||
| 著者所属 | Earthquake Research Institute. | |||||
| 抄録 | ||||||
| 内容記述タイプ | Abstract | |||||
| 内容記述 | The main revised results are as follows : (1) The amplitudes of the radial component of the displacement of the dilatational waves at a distant point have maximum values at certain ha's in both single and quadruple sources. (2) The amplitudes of the dilatational waves at a distant point in the two cases vanish when the wave lengths are very long compared with the dimension of the origin. (3) The amplitude of the dilatational wave generated from the quadruple source becomes appoximately equal to that from the single source when ha>4, as the result of the fact that the distortional waves appear less and less intensely than the dilatational waves when the wave length diminishes as compared with the size of the seismic origin. (4) In the case where the normal pressure at the origin is expressed by two zonal harmonics P0(cosθ) and P2(cosθ), so long as the wave length is greater than the radius of the seismic origin, the component due to the term P0(cosθ) is greater than that due to the term P2(cosθ). Should the wave length become comparable with the dimension of the seismic origin, we find that the azimuthal distribution of the displacement of the dilatational wave becomes quite similar to the azimuthal distribution in the pressure at the seismic origin. (5) Although we cannot, from the mere results of these calculations, say anything conclusive regarding the wave length of such waves as might be generated from a seismic origin, the writer considers it preferable to think that waves might be generated having wave lengths comparable with the size of the origin than to think that the wave lengths of the waves are very much longer than the dimension of the seismic origin, (see summary of my ""Notes on the Origins of Earthquakes, second paper."") | |||||
| 書誌情報 |
東京帝國大學地震研究所彙報 = Bulletin of the Earthquake Research Institute, Tokyo Imperial University 巻 15, 号 4, p. 956-964, 発行日 1937-12-20 |
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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 | AN00029699 | |||||
| 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 | 東京帝国大学地震研究所 | |||||
| 出版者別名 | ||||||
| Earthquake Research Institute, Tokyo Imperial University | ||||||
