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Recent Activity of Volcano Sakura-zima, (Ⅱ)"}]}, "item_4_biblio_info_7": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1948-06-30", "bibliographicIssueDateType": "Issued"}, "bibliographicIssueNumber": "1-4", "bibliographicPageEnd": "184", "bibliographicPageStart": "179", "bibliographicVolumeNumber": "24", "bibliographic_titles": [{"bibliographic_title": "東京大學地震研究所彙報 = Bulletin of the Earthquake Research Institute, University of Tokyo"}]}]}, "item_4_description_13": {"attribute_name": "フォーマット", "attribute_value_mlt": [{"subitem_description": "application/pdf", "subitem_description_type": "Other"}]}, "item_4_description_5": {"attribute_name": "抄録", "attribute_value_mlt": [{"subitem_description": "A survey of geomagnetic dip was repeated by the dip circle used in the first survey in 1939. Remarkable changes in dip were not observed at any place in the Sakura-zima Island but one situated quite near the new lavaflow. 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13. 最近の櫻島火山の活動に就いて(Ⅱ) : 新熔岩流の帶磁と傾斜變化
https://doi.org/10.15083/0000034303
https://doi.org/10.15083/00000343035905c796-cf36-4880-90e2-50f06035867d
名前 / ファイル | ライセンス | アクション |
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ji0241013.pdf (351.0 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 | 13. 最近の櫻島火山の活動に就いて(Ⅱ) : 新熔岩流の帶磁と傾斜變化 | |||||
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 | 10.15083/0000034303 | |||||
ID登録タイプ | JaLC | |||||
その他のタイトル | ||||||
その他のタイトル | 13. Recent Activity of Volcano Sakura-zima, (Ⅱ) | |||||
著者 |
水上, 武
× 水上, 武× 佐久間, 修三 |
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著者別名 | ||||||
識別子 | 133369 | |||||
識別子Scheme | WEKO | |||||
姓名 | Minakami, Takeshi | |||||
著者別名 | ||||||
識別子 | 133370 | |||||
識別子Scheme | WEKO | |||||
姓名 | Sakuma, Shuzo | |||||
著者所属 | ||||||
著者所属 | 地震研究所 | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | A survey of geomagnetic dip was repeated by the dip circle used in the first survey in 1939. Remarkable changes in dip were not observed at any place in the Sakura-zima Island but one situated quite near the new lavaflow. By another dip-survey across the north side of the newlava, it was found that the lava was magnetized in the direction of the present geomagnetic field as a whole, and its intensity of magnetization calculated from the observed anomaly was 0.005±0.001 e.m.u. Measurement of tilt of the ground was also repeated in the same manner as in April. Most of bench-marks having bean destroyed, during Apr.~Oct., only three groups of them remained. At these stations, the ground tilted towards the same direction as before(See Fig.4), and its daily rate of the tilt decreased to 1/9 of that of April. The topographic distribution of direction of tilt suggests that the island consists of more than three blocks. A topographic survey near the new crater was carried out by a mountain barometer and a clinometer. | |||||
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. 179-184, 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 | 453 | |||||
主題Scheme | NDC | |||||
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 |