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17. 櫻島に於ける地球磁氣觀測結果及び新熔岩の磁氣的性質
https://doi.org/10.15083/0000034307
https://doi.org/10.15083/00000343076c5731ce-bcae-46b9-ad43-f9645dca3c81
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
ji0241017.pdf (491.0 kB)
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| Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
|---|---|---|---|---|---|---|
| 公開日 | 2008-06-06 | |||||
| タイトル | ||||||
| タイトル | 17. 櫻島に於ける地球磁氣觀測結果及び新熔岩の磁氣的性質 | |||||
| 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 | 10.15083/0000034307 | |||||
| ID登録タイプ | JaLC | |||||
| その他のタイトル | ||||||
| その他のタイトル | 17. The Result of Geomagnetic Study on the Latest Eruption of Sakurazima and Magnetic Properties of the New Ejecta | |||||
| 著者 |
原田, 美道
× 原田, 美道× 畠山, 勉× 大林, 辰藏 |
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| 著者別名 | ||||||
| 識別子Scheme | WEKO | |||||
| 識別子 | 133390 | |||||
| 姓名 | Harada, Y. | |||||
| 著者別名 | ||||||
| 識別子Scheme | WEKO | |||||
| 識別子 | 133391 | |||||
| 姓名 | Hatakeyama, T. | |||||
| 著者別名 | ||||||
| 識別子Scheme | WEKO | |||||
| 識別子 | 133392 | |||||
| 姓名 | Obayasi, T. | |||||
| 著者所属 | ||||||
| 著者所属 | 地球物理學敎室 | |||||
| 抄録 | ||||||
| 内容記述タイプ | Abstract | |||||
| 内容記述 | On March 9, 1946. Volcanic island Sakurazima began its activity. The writers measured the anomalous magnetic field and its changes on the volcanic island, Sakurazima, during the period of March 23 to April 17. The chief results are as follows. (1) The local anomaly of geomagnetic declination, D, due to the magnetization of the Sakurazima is shown in Fig.2. Assuming that the specific intensity of magnetization J is equal to that of the natural residual magnetization Jn, we get the equation of the anomaly of the declination as, tg ΔD=-0.004sinΦ-0.026sin2Φ. In this equation, if we make some corrections of the observed values we can find that the observed values of D are well expressed in this equation. From this fact, it may be said that the direction of the magnetization agrees with that of the present meridian, and that a part of this magnetization of Sakurazima, for the most part, is due to the presence of the natural remanent magnetization in rock. (2) The result of the measuring of the magnetic properties of the newly ejected lava are shown in Table.I-2, I-3. The average value of specific susceptibility is about 0.98×10^<-3>, while that of natural residual magnetization is Jn～6.0×10^<-3> e.m.u., these values being fairly. smaller than those of basaltic rocks. (3) Although it has been reported that there was some remarkable magnetic. changes accompanying eruption of volcanoes, Asama and Mihara, we could find no changes in both of ΔD and ΔH in the case of presenteruption of Sakurazima. This fact may suggest us that there is some necessary conditions for anomalous changes in geomagnetic field accompanying volcanic eruption, such, for example, as the ""magnetizibility"" which is usually predominant in the basaltic rocks. | |||||
| 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 24, 号 1-4, p. 207-216, 発行日 1948-06-30 |
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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 | ||||||
| Earthquake Research Institute, University of Tokyo | ||||||
