{"created":"2021-03-01T06:53:19.297601+00:00","id":34427,"links":{},"metadata":{"_buckets":{"deposit":"fe2ddbba-5631-44ca-b678-ba825cfbbbb0"},"_deposit":{"id":"34427","owner":"1","owners":[],"pid":{"revision_id":0,"type":"depid","value":"34427"},"status":"published"},"_oai":{"id":"oai:repository.dl.itc.u-tokyo.ac.jp:00034427","sets":["80:4535:5147:5155","9:504:4538:5149:5156"]},"author_link":["133697","133698","133695","133696"],"item_4_alternative_title_1":{"attribute_name":"その他のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"重力異常と地下構造との關係(VI.)"}]},"item_4_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1941-03-30","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"1","bibliographicPageEnd":"38","bibliographicPageStart":"26","bibliographicVolumeNumber":"19","bibliographic_titles":[{"bibliographic_title":"東京帝國大學地震研究所彙報 = Bulletin of the Earthquake Research Institute, Tokyo Imperial University"}]}]},"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":"蘭領東インド諸島の東半分に於ける重力異常を材料とし,二重Fourier級數を利用して此の地域の地下構造を論じた.其の結果を要約すれば次の通りである. 1. Airy均衡地殻の厚さは32 km である, 2. 地方的均衡の極限は80kmである. 3. 均衡ジオイドは最大20mも凹んで居る. 4. 一般に地方的均衡の極限は均衡地殻の厚さの2～3倍であるらしい.","subitem_description_type":"Abstract"}]},"item_4_full_name_3":{"attribute_name":"著者別名","attribute_value_mlt":[{"nameIdentifiers":[{"nameIdentifier":"133697","nameIdentifierScheme":"WEKO"}],"names":[{"name":"坪井, 忠二"}]},{"nameIdentifiers":[{"nameIdentifier":"133698","nameIdentifierScheme":"WEKO"}],"names":[{"name":"山口, 生知"}]}]},"item_4_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.15083/0000034427","subitem_identifier_reg_type":"JaLC"}]},"item_4_publisher_20":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"東京帝国大学地震研究所"}]},"item_4_source_id_10":{"attribute_name":"書誌レコードID","attribute_value_mlt":[{"subitem_source_identifier":"AN00029699","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, Tokyo Imperial University"}]},"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":"Tsuboi, Chuji"}],"nameIdentifiers":[{"nameIdentifier":"133695","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"Yamaguti, Seiti"}],"nameIdentifiers":[{"nameIdentifier":"133696","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":"ji0191004.pdf","filesize":[{"value":"640.4 kB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"ji0191004.pdf","url":"https://repository.dl.itc.u-tokyo.ac.jp/record/34427/files/ji0191004.pdf"},"version_id":"7e906379-da55-4297-8266-848a58c10ba6"}]},"item_language":{"attribute_name":"言語","attribute_value_mlt":[{"subitem_language":"eng"}]},"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":"Relation between the Gravity Anomalies and the Corresponding Subterranean Mass Distribution. (VI.)","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"Relation between the Gravity Anomalies and the Corresponding Subterranean Mass Distribution. (VI.)","subitem_title_language":"en"}]},"item_type_id":"4","owner":"1","path":["5155","5156"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2008-06-06"},"publish_date":"2008-06-06","publish_status":"0","recid":"34427","relation_version_is_last":true,"title":["Relation between the Gravity Anomalies and the Corresponding Subterranean Mass Distribution. (VI.)"],"weko_creator_id":"1","weko_shared_id":-1},"updated":"2022-12-19T04:58:39.935620+00:00"}