{"created":"2021-03-01T06:53:10.985998+00:00","id":34303,"links":{},"metadata":{"_buckets":{"deposit":"b4bbdfdc-2c9a-4c22-82b5-140fc530ae81"},"_deposit":{"id":"34303","owner":"1","owners":[],"pid":{"revision_id":0,"type":"depid","value":"34303"},"status":"published"},"_oai":{"id":"oai:repository.dl.itc.u-tokyo.ac.jp:00034303","sets":["80:4535:5115:5116","9:504:4538:5117:5118"]},"author_link":["133369","133370","133367","133368"],"item_4_alternative_title_1":{"attribute_name":"その他のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"13. 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. 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.","subitem_description_type":"Abstract"}]},"item_4_full_name_3":{"attribute_name":"著者別名","attribute_value_mlt":[{"nameIdentifiers":[{"nameIdentifier":"133369","nameIdentifierScheme":"WEKO"}],"names":[{"name":"Minakami, Takeshi"}]},{"nameIdentifiers":[{"nameIdentifier":"133370","nameIdentifierScheme":"WEKO"}],"names":[{"name":"Sakuma, Shuzo"}]}]},"item_4_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.15083/0000034303","subitem_identifier_reg_type":"JaLC"}]},"item_4_publisher_20":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"東京大学地震研究所"}]},"item_4_source_id_10":{"attribute_name":"書誌レコードID","attribute_value_mlt":[{"subitem_source_identifier":"AN00162258","subitem_source_identifier_type":"NCID"}]},"item_4_source_id_8":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"00408972","subitem_source_identifier_type":"ISSN"}]},"item_4_subject_15":{"attribute_name":"日本十進分類法","attribute_value_mlt":[{"subitem_subject":"453","subitem_subject_scheme":"NDC"}]},"item_4_text_21":{"attribute_name":"出版者別名","attribute_value_mlt":[{"subitem_text_value":"Earthquake Research Institute, University of Tokyo"}]},"item_4_text_4":{"attribute_name":"著者所属","attribute_value_mlt":[{"subitem_text_value":"地震研究所"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"水上, 武"}],"nameIdentifiers":[{"nameIdentifier":"133367","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"佐久間, 修三"}],"nameIdentifiers":[{"nameIdentifier":"133368","nameIdentifierScheme":"WEKO"}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2017-06-27"}],"displaytype":"detail","filename":"ji0241013.pdf","filesize":[{"value":"351.0 kB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"ji0241013.pdf","url":"https://repository.dl.itc.u-tokyo.ac.jp/record/34303/files/ji0241013.pdf"},"version_id":"b633dac9-a5f2-4464-b02f-98256483cf8a"}]},"item_language":{"attribute_name":"言語","attribute_value_mlt":[{"subitem_language":"jpn"}]},"item_resource_type":{"attribute_name":"資源タイプ","attribute_value_mlt":[{"resourcetype":"departmental bulletin paper","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_title":"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","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"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","subitem_title_language":"ja"}]},"item_type_id":"4","owner":"1","path":["5116","5118"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2008-06-06"},"publish_date":"2008-06-06","publish_status":"0","recid":"34303","relation_version_is_last":true,"title":["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"],"weko_creator_id":"1","weko_shared_id":-1},"updated":"2022-12-19T04:09:23.716302+00:00"}