{"created":"2021-03-01T06:51:14.278228+00:00","id":32554,"links":{},"metadata":{"_buckets":{"deposit":"05fdac14-447f-42ba-944b-ed276f03c5ce"},"_deposit":{"id":"32554","owner":"1","owners":[],"pid":{"revision_id":0,"type":"depid","value":"32554"},"status":"published"},"_oai":{"id":"oai:repository.dl.itc.u-tokyo.ac.jp:00032554","sets":["80:4535:4619:4623","9:504:4538:4621:4624"]},"author_link":["125583","125582"],"item_4_alternative_title_1":{"attribute_name":"その他のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"Cycle of Interplate Earthquake Along the Sagami Trough, Deduced from Tectonic Geomorphology"}]},"item_4_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2003","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"3","bibliographicPageEnd":"254","bibliographicPageStart":"245","bibliographicVolumeNumber":"78","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 tectonic geomorphological study is one of the best methods of evaluating the timing and the crustal deformation of pre-historic earthquake. To reveal the cycle of interplate earthquakes along the Sagami Trough, I investigatedthe emergedshoreline topography andthe fossilizedsessile assemblages in the Miura Peninsula andthe Boso Peninsula. The distribution pattern of coseismic vertical displacement during the 1703 Genroku Kanto Earthquake inferredfrom the height distribution of the paleo-shoreline suggests that the fault source model consists of a dual fault system of the Fault A andB. Fault A is also the source of the 1923 Taisho Kanto Earthquake. The geometry and ages of the emerged shoreline topography divided into several levels indicate that the characteristic earthquake generatedfrom Fault A has occurredabout every 400 years. One of several events, it is accompaniedwith a slip of Fault B, which has a recurrence interval of 2000-2700 years.","subitem_description_type":"Abstract"}]},"item_4_full_name_3":{"attribute_name":"著者別名","attribute_value_mlt":[{"nameIdentifiers":[{"nameIdentifier":"125583","nameIdentifierScheme":"WEKO"}],"names":[{"name":"Shishikura, Masanobu"}]}]},"item_4_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.15083/0000032554","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":"51.1","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":"産業技術総合研究所活断層研究センター"},{"subitem_text_value":"Active Fault Reserch Center, GSJ/AIST"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"宍倉, 正展"}],"nameIdentifiers":[{"nameIdentifier":"125582","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":"IHO78303.pdf","filesize":[{"value":"6.5MB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"IHO78303.pdf","url":"https://repository.dl.itc.u-tokyo.ac.jp/record/32554/files/IHO78303.pdf"},"version_id":"b317b4b7-4d54-4648-a5fc-87fc01a8b179"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"tectonic geomorphology","subitem_subject_scheme":"Other"},{"subitem_subject":"paleo-shoreline","subitem_subject_scheme":"Other"},{"subitem_subject":"recurrence interval","subitem_subject_scheme":"Other"},{"subitem_subject":"Sagami Trough","subitem_subject_scheme":"Other"},{"subitem_subject":"Kanto Earthquake","subitem_subject_scheme":"Other"}]},"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":"変動地形からみた相模トラフにおけるプレート間地震サイクル","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"変動地形からみた相模トラフにおけるプレート間地震サイクル","subitem_title_language":"ja"}]},"item_type_id":"4","owner":"1","path":["4623","4624"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2007-04-23"},"publish_date":"2007-04-23","publish_status":"0","recid":"32554","relation_version_is_last":true,"title":["変動地形からみた相模トラフにおけるプレート間地震サイクル"],"weko_creator_id":"1","weko_shared_id":-1},"updated":"2022-12-19T04:08:36.429055+00:00"}