{"created":"2023-07-27T06:51:58.826559+00:00","id":45633,"links":{},"metadata":{"_buckets":{"deposit":"de2abf04-b452-4ad1-aee4-a1de761dafba"},"_deposit":{"created_by":18,"id":"45633","owners":[18],"pid":{"revision_id":0,"type":"depid","value":"45633"},"status":"published"},"_oai":{"id":"oai:kanazawa-u.repo.nii.ac.jp:00045633","sets":["2812:2813:2818"]},"author_link":["17381","229"],"item_9_biblio_info_8":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2016-06-14","bibliographicIssueDateType":"Issued"},"bibliographicPageStart":"6p.","bibliographicVolumeNumber":"2012-04-01 - 2016-03-31","bibliographic_titles":[{"bibliographic_title":"平成27(2015)年度 科学研究費補助金 基盤研究(B) 研究成果報告書"},{"bibliographic_title":"2015 Fiscal Year Final Research Report","bibliographic_titleLang":"en"}]}]},"item_9_creator_33":{"attribute_name":"著者別表示","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{}],"nameIdentifiers":[{},{}]}]},"item_9_description_21":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"南海沈み込み境界の巨大地震発生域周縁に観測されるゆっくり滑りの不均質の地質学的実態と成因を理解するため、上盤マントルの蛇紋岩化の岩石学的モデルに基づき、構造地質学と地球物理学と地形年代学による多角的アプローチから検証に取り組んだ。その結果（１）ゆっくり滑りに伴う深部低周波微動と天然蛇紋岩構造がサイズ分布において対比できること、（２）四国西部の重力異常の東西変化や深部低周波微動の特徴的な長さの東西変化が蛇紋岩化の違いで説明できる可能性、（３）四国の河川の離水年代からプレート界面不均質への地殻応答が制約できる可能性が見えた。プレート境界深部の歪み解消過程の定量化へ一つの道筋をつける成果と言える。","subitem_description_type":"Abstract"},{"subitem_description":"Slow slips at subduction boundaries are considered to be critical in stress build-up on the megathrust zones. We examine petrological controls on the mechanism and heterogeneous distribution of slip sources using multidisciplinary approaches including structural geology, geophysics and geomorphological chronology. The following results on the Nankai subduction zone will be an important step for practical understanding of slow slip phenomena: Layered structures of antigorite serpentinite formed through open system crust-mantle interaction show an exponential scaling relationship similar to deep low frequency tremors (DLFTs); The lateral variation in gravitational anomaly and scaling relationship between duration and amplitude of DLFTs can be explained by variable extents of serpentinization consistent with the present thermal structure of the Nankai region; Water separation ages successfully constrain the development of the Shimanto River system in response to the plate coupling.","subitem_description_type":"Abstract"}]},"item_9_description_22":{"attribute_name":"内容記述","attribute_value_mlt":[{"subitem_description":"研究課題/領域番号:24340122, 研究期間(年度):2012-04-01 - 2016-03-31","subitem_description_type":"Other"},{"subitem_description":"出典：研究課題「南海プレート境界の不均質すべりと前弧テクトニクスの相関抽出」課題番号24340122\n（KAKEN：科学研究費助成事業データベース（国立情報学研究所）） \n（https://kaken.nii.ac.jp/report/KAKENHI-PROJECT-24340122/24340122seika/）を加工して作成","subitem_description_type":"Other"}]},"item_9_description_5":{"attribute_name":"提供者所属","attribute_value_mlt":[{"subitem_description":"金沢大学理工研究域地球社会基盤学系","subitem_description_type":"Other"}]},"item_9_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.24517/00051970","subitem_identifier_reg_type":"JaLC"}]},"item_9_relation_28":{"attribute_name":"関連URI","attribute_value_mlt":[{"subitem_relation_name":[{"subitem_relation_name_text":"https://kaken.nii.ac.jp/search/?qm=80396811"}],"subitem_relation_type_id":{"subitem_relation_type_id_text":"https://kaken.nii.ac.jp/search/?qm=80396811","subitem_relation_type_select":"URI"}},{"subitem_relation_name":[{"subitem_relation_name_text":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-24340122/"}],"subitem_relation_type_id":{"subitem_relation_type_id_text":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-24340122/","subitem_relation_type_select":"URI"}},{"subitem_relation_name":[{"subitem_relation_name_text":"https://kaken.nii.ac.jp/report/KAKENHI-PROJECT-24340122/24340122seika/"}],"subitem_relation_type_id":{"subitem_relation_type_id_text":"https://kaken.nii.ac.jp/report/KAKENHI-PROJECT-24340122/24340122seika/","subitem_relation_type_select":"URI"}}]},"item_9_version_type_25":{"attribute_name":"著者版フラグ","attribute_value_mlt":[{"subitem_version_resource":"http://purl.org/coar/version/c_ab4af688f83e57aa","subitem_version_type":"AM"}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2018-08-23"}],"displaytype":"detail","filename":"SC-PR-MIZUKAMI-T-kaken 2016-6p.pdf","filesize":[{"value":"326.9 kB"}],"format":"application/pdf","licensetype":"license_11","mimetype":"application/pdf","url":{"label":"SC-PR-MIZUKAMI-T-kaken 2016-6p.pdf","url":"https://kanazawa-u.repo.nii.ac.jp/record/45633/files/SC-PR-MIZUKAMI-T-kaken 2016-6p.pdf"},"version_id":"9ea1d799-ff1d-4e17-82ac-99f5740304c2"}]},"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":"research report","resourceuri":"http://purl.org/coar/resource_type/c_18ws"}]},"item_title":"南海プレート境界の不均質すべりと前弧テクトニクスの相関抽出","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"南海プレート境界の不均質すべりと前弧テクトニクスの相関抽出"},{"subitem_title":"Examination of tectonic relationships between heterogeneous slow slip behaviors and forearc deformation in the Nankai subduction zone","subitem_title_language":"en"}]},"item_type_id":"9","owner":"18","path":["2818"],"pubdate":{"attribute_name":"公開日","attribute_value":"2018-08-23"},"publish_date":"2018-08-23","publish_status":"0","recid":"45633","relation_version_is_last":true,"title":["南海プレート境界の不均質すべりと前弧テクトニクスの相関抽出"],"weko_creator_id":"18","weko_shared_id":-1},"updated":"2023-07-27T10:54:38.855130+00:00"}