{"created":"2021-03-01T06:52:05.479999+00:00","id":33323,"links":{},"metadata":{"_buckets":{"deposit":"5b70b5ee-753c-4e67-95fd-0119c93dcc50"},"_deposit":{"id":"33323","owner":"1","owners":[],"pid":{"revision_id":0,"type":"depid","value":"33323"},"status":"published"},"_oai":{"id":"oai:repository.dl.itc.u-tokyo.ac.jp:00033323","sets":["80:4535:4885:4895","9:504:4538:4887:4896"]},"author_link":["130111","130110"],"item_4_alternative_title_1":{"attribute_name":"その他のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"9.世界の特殊な地震活動地区について : その4 ニューブリテソ諸島周辺"}]},"item_4_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1970-06-10","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"2","bibliographicPageEnd":"143","bibliographicPageStart":"127","bibliographicVolumeNumber":"48","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":"Character of seismicity in New Britain Island region was investigated by using the data of U. S. Coast and Geodetic Survey during the period from January 1963 to July 1969. There were three parallel seismic zones running in an E-W direction. Earthquakes along the northernmost and southernmost zones were limited to shallow ones. Foci distributions in the central seismic zone along the profiles perpendicular to the trench showed a trench-island arc system. They were expressed by the same curve excepting one along a profile crossing the Bougainville Island. In the latter profile, foci were dispersed to such an extent that no focal zone could be recognized, and there occurred upper mantle events even just beneath the axis of the trench. In the central zone, swarms and aftershocks were quite active. Large earthquakes have historically been active along this zone only. These features are common with the seismicity along an arc from New Hebrides to New Guinea. Their foci in New Britain Island region, however, were found to penetrate deeper. A special concern was given upon the existence of a northernmost shallow seismic zone running through the Bismarck Sea.|1963年1月から1969年7月までの7年7ケ月の期間中にニューブリテン諸島周辺で起こつた地震について,今まで同様,USCGSの資料をそのまま用いて,その活動の特徴を調べた.","subitem_description_type":"Abstract"}]},"item_4_full_name_3":{"attribute_name":"著者別名","attribute_value_mlt":[{"nameIdentifiers":[{"nameIdentifier":"130111","nameIdentifierScheme":"WEKO"}],"names":[{"name":"三東, 哲夫"}]}]},"item_4_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.15083/0000033323","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":"Earthquake Research Institute"},{"subitem_text_value":"International Institute of Seismology and Earthquake Engineering"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"Santo, Tetsuo"}],"nameIdentifiers":[{"nameIdentifier":"130110","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":"2017-06-26"}],"displaytype":"detail","filename":"ji0482003.pdf","filesize":[{"value":"1.0 MB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"ji0482003.pdf","url":"https://repository.dl.itc.u-tokyo.ac.jp/record/33323/files/ji0482003.pdf"},"version_id":"1e1dbbf4-aa32-44eb-9df6-916608588b78"}]},"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":"9. Regional Study on the Characteristic Seismicity of the World : Part 4. New Britain Island Region","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"9. Regional Study on the Characteristic Seismicity of the World : Part 4. New Britain Island Region","subitem_title_language":"en"}]},"item_type_id":"4","owner":"1","path":["4895","4896"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2008-05-30"},"publish_date":"2008-05-30","publish_status":"0","recid":"33323","relation_version_is_last":true,"title":["9. Regional Study on the Characteristic Seismicity of the World : Part 4. New Britain Island Region"],"weko_creator_id":"1","weko_shared_id":-1},"updated":"2022-12-19T04:37:06.969978+00:00"}