{"created":"2021-03-01T06:17:19.887308+00:00","id":783,"links":{},"metadata":{"_buckets":{"deposit":"13430d71-90b5-4740-ab11-1cd39b7f19d9"},"_deposit":{"id":"783","owners":[],"pid":{"revision_id":0,"type":"depid","value":"783"},"status":"published"},"_oai":{"id":"oai:repository.dl.itc.u-tokyo.ac.jp:00000783","sets":["80:115:116","9:10:11"]},"item_2_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2008-10-20","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"3","bibliographicPageEnd":"1163","bibliographicPageStart":"1153","bibliographicVolumeNumber":"169","bibliographic_titles":[{"bibliographic_title":"Geophysical journal international"}]}]},"item_2_description_5":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"A whole mantle SH velocity model is obtained by using a unique data set and techniques. Body and surface waveforms including major and multi-orbit phases are used as a data set and are inverted by using 3-D Born kernels. The resultant model, SH18CE, reveals the different natures of the two major upwelling systems: the strong low velocity anomalies beneath Africa extend for more than 1000 km from the core-mantle boundary (CMB), whereas those beneath the Pacific are restricted to 300-400 km from the CMB. The results also show the variable natures of stagnant slabs on the 670 discontinuity around Japan: the depths of the strongest high velocity anomalies within the stagnant slabs are different region by region, which is consistent with the detailed delay time tomography model in this area.","subitem_description_type":"Abstract"}]},"item_2_publisher_20":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"Blackwell Scientific Publications"}]},"item_2_relation_11":{"attribute_name":"DOI","attribute_value_mlt":[{"subitem_relation_type_id":{"subitem_relation_type_id_text":"info:doi/10.1111/j.1365-246X.2007.03405.x","subitem_relation_type_select":"DOI"}}]},"item_2_relation_25":{"attribute_name":"関係URI","attribute_value_mlt":[{"subitem_relation_type_id":{"subitem_relation_type_id_text":"http://www.blackwell-synergy.com","subitem_relation_type_select":"URI"}}]},"item_2_rights_12":{"attribute_name":"権利","attribute_value_mlt":[{"subitem_rights":"The definitive version is available at www.blackwell-synergy.com"}]},"item_2_select_14":{"attribute_name":"著者版フラグ","attribute_value_mlt":[{"subitem_select_item":"author"}]},"item_2_source_id_10":{"attribute_name":"書誌レコードID","attribute_value_mlt":[{"subitem_source_identifier":"AA10717798","subitem_source_identifier_type":"NCID"}]},"item_2_source_id_8":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"0956540X","subitem_source_identifier_type":"ISSN"}]},"item_2_subject_15":{"attribute_name":"日本十進分類法","attribute_value_mlt":[{"subitem_subject":"450","subitem_subject_scheme":"NDC"}]},"item_2_text_4":{"attribute_name":"著者所属","attribute_value_mlt":[{"subitem_text_value":"Earthquake Research Institute, University of Tokyo"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"Takeuchi, Nozomu"}],"nameIdentifiers":[{"nameIdentifier":"2998","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":"2017-05-30"}],"displaytype":"detail","filename":"takeuchi_2007GJI.pdf","filesize":[{"value":"4.2 MB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"takeuchi_2007GJI.pdf","url":"https://repository.dl.itc.u-tokyo.ac.jp/record/783/files/takeuchi_2007GJI.pdf"},"version_id":"589419b9-e148-4ad3-890b-4b11dad2b8ee"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"Global seismology","subitem_subject_scheme":"Other"},{"subitem_subject":"Inversion","subitem_subject_scheme":"Other"},{"subitem_subject":"Seismic structure","subitem_subject_scheme":"Other"},{"subitem_subject":"Tomography","subitem_subject_scheme":"Other"},{"subitem_subject":"Direct Solution Method","subitem_subject_scheme":"Other"}]},"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":"journal article","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_title":"Whole mantle SH velocity model constrained by waveform inversion based on three-dimensional Born kernels","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"Whole mantle SH velocity model constrained by waveform inversion based on three-dimensional Born kernels"}]},"item_type_id":"2","owner":"1","path":["11","116"],"pubdate":{"attribute_name":"公開日","attribute_value":"2017-01-05"},"publish_date":"2017-01-05","publish_status":"0","recid":"783","relation_version_is_last":true,"title":["Whole mantle SH velocity model constrained by waveform inversion based on three-dimensional Born kernels"],"weko_creator_id":"1","weko_shared_id":null},"updated":"2022-12-19T03:41:50.226240+00:00"}