{"created":"2023-07-27T07:00:12.576008+00:00","id":60053,"links":{},"metadata":{"_buckets":{"deposit":"5e621676-5899-4a69-a121-b3c0aad048cf"},"_deposit":{"created_by":3,"id":"60053","owners":[3],"pid":{"revision_id":0,"type":"depid","value":"60053"},"status":"published"},"_oai":{"id":"oai:kanazawa-u.repo.nii.ac.jp:00060053","sets":["1979:1982:1983:4107"]},"author_link":["105736","105737","105732","105738","105734","105735","105731","105729","105730","105733"],"item_7_biblio_info_8":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2022-03-22","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"50","bibliographicPageStart":"41","bibliographicVolumeNumber":"53","bibliographic_titles":[{"bibliographic_title":"日本海域研究"},{"bibliographic_title":"Japan sea research","bibliographic_titleLang":"en"}]}]},"item_7_creator_34":{"attribute_name":"著者別表示","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"SAWADA, Akihiro"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"ISHIDA, Satoshi"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"KOBAYASHI, Wataru"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"NOHARA, Koji"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"HIRAMATSU, Yoshihiro"}],"nameIdentifiers":[{}]}]},"item_7_description_21":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"In the sea area off the west coast of the Noto Peninsula, there are faults and flexures that have been formed since the Tertiary Period. It is also the area in which the magnitude 6.9 Noto Hanto earthquake occurred on March 25th 2007. Many acoustic surveys have been carried out and have revealed the vertical cross-sections of subsurface sedimentary structures in this area. In this study, we compiled the boundary depths of the sedimentary structures, together with the distribution of faults and flexures, and created a three-dimensional (3D) depth distribution of the boundaries of the subsurface geological structures formed since the Tertiary Period in this area. The obtained 3D depth distribution of the boundaries illuminates the distribution of the flexure structure in the sea area off the city of Hakui at each boundary. We recognized that the boundary depths change steeply for the Quaternary Period reverse faults that lie relatively close to the coast, while little for the faults far from the coast.","subitem_description_type":"Abstract"}]},"item_7_heading_33":{"attribute_name":"見出し","attribute_value_mlt":[{"subitem_heading_banner_headline":"資料","subitem_heading_language":"ja"}]},"item_7_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.24517/00066304","subitem_identifier_reg_type":"JaLC"}]},"item_7_publisher_17":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"金沢大学環日本海域環境研究センター "}]},"item_7_publisher_19":{"attribute_name":"出版者（別名）","attribute_value_mlt":[{"subitem_publisher":"Institute of Nature and Environmental Technology Kanazawa University"}]},"item_7_source_id_11":{"attribute_name":"NCID","attribute_value_mlt":[{"subitem_source_identifier":"AA11430153","subitem_source_identifier_type":"NCID"}]},"item_7_source_id_9":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"1347-7889","subitem_source_identifier_type":"ISSN"}]},"item_7_version_type_25":{"attribute_name":"著者版フラグ","attribute_value_mlt":[{"subitem_version_resource":"http://purl.org/coar/version/c_970fb48d4fbd8a85","subitem_version_type":"VoR"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"澤田, 明宏"}],"nameIdentifiers":[{"nameIdentifier":"105729","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"石田, 聡史"}],"nameIdentifiers":[{"nameIdentifier":"105730","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"小林, 航"}],"nameIdentifiers":[{"nameIdentifier":"105731","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"野原, 幸嗣"}],"nameIdentifiers":[{"nameIdentifier":"105732","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"平松, 良浩"}],"nameIdentifiers":[{"nameIdentifier":"105733","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":"2022-06-03"}],"displaytype":"detail","filename":"AA11430153-53-41-50.pdf","filesize":[{"value":"1.7 MB"}],"format":"application/pdf","licensetype":"license_11","mimetype":"application/pdf","url":{"label":"AA11430153-53-41-50.pdf","url":"https://kanazawa-u.repo.nii.ac.jp/record/60053/files/AA11430153-53-41-50.pdf"},"version_id":"35a7d482-cfbb-4ba8-88c4-754557fbb759"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"音波探査","subitem_subject_scheme":"Other"},{"subitem_subject":"第四紀","subitem_subject_scheme":"Other"},{"subitem_subject":"活断層","subitem_subject_scheme":"Other"},{"subitem_subject":"撓曲，深度分布","subitem_subject_scheme":"Other"},{"subitem_subject":"acoustic survey","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"active fault","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"depth distributionflexure","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"Noto Peninsula","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"Quaternary Period","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"Tertiary Period","subitem_subject_language":"en","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":"能登半島西方海域における3次元地質構造モデル","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"能登半島西方海域における3次元地質構造モデル"},{"subitem_title":"A Model of a 3-Dimensional Geological Structure off the West Coast of the Noto Peninsula, the Sea of Japan","subitem_title_language":"en"}]},"item_type_id":"7","owner":"3","path":["4107"],"pubdate":{"attribute_name":"公開日","attribute_value":"2022-06-03"},"publish_date":"2022-06-03","publish_status":"0","recid":"60053","relation_version_is_last":true,"title":["能登半島西方海域における3次元地質構造モデル"],"weko_creator_id":"3","weko_shared_id":3},"updated":"2023-07-27T12:55:37.560892+00:00"}