{"created":"2023-07-27T06:51:57.090923+00:00","id":45589,"links":{},"metadata":{"_buckets":{"deposit":"5bfefdf8-fee9-40fc-a934-d4bfacf0ed52"},"_deposit":{"created_by":18,"id":"45589","owners":[18],"pid":{"revision_id":0,"type":"depid","value":"45589"},"status":"published"},"_oai":{"id":"oai:kanazawa-u.repo.nii.ac.jp:00045589","sets":["2812:2813:2817"]},"author_link":["17481","2310"],"item_9_biblio_info_8":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2017-06-20","bibliographicIssueDateType":"Issued"},"bibliographicPageStart":"4p.","bibliographicVolumeNumber":"2014-04-01 - 2017-03-31","bibliographic_titles":[{"bibliographic_title":"平成28(2016)年度 科学研究費補助金 基盤研究(B) 研究成果報告書"},{"bibliographic_title":"2016 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":"海洋プレート下マントルの成因と履歴に関する本研究成果は，１）中央海嶺かんらん岩に太古溶融物質混入の可能性の指摘、メルトーかんらん岩反応による枯渇したかんらん岩の地殻化プロセスの提言,２）ジュラ紀から白亜紀に形成された海洋プレートであるテチス海オフィオライトの東部に位置するアンダマンオフィオライトのマントルセクションの特徴を中央海嶺下で形成されたかんらん岩と特定し，海洋プレートから島弧形成プロセス初期過程を解明，３）背弧である日本海の火山岩中のカンラン岩捕獲岩の検討から，中央海嶺下に類似下マグマプロセスが起きていることを明らかにした。","subitem_description_type":"Abstract"},{"subitem_description":"Results of this research on the sub-oceanic mantle peridotites are summarized as follows. 1)　We suggested possibility of existence of ancient melted residue in abyssal peridotites recovered from mid-ocean ridge system (Indian Ocean) and its “crustallization” processes by melt-residual peridotite interactions. Addition to this, melting processes selectively accumulated ancient melting geochemical signatures by melt-rock interactions. 2) We clarified mid-ocean ridge type peridotite origin for mantle section of the Eastern end of the Jurassic-Cretaceous ophiolite belt (Tethys ophiolite belt), Andaman Ophiolite, and its modification at subduction setting during the initiation of subduction. 3) We examined back-arc magmatic processes deduced from peridotite xenolith in back arc region (Japan Sea). Our results suggest that the late stage of magma process is similar to those expected beneath Mid-ocean ridge setting, resulting in the similar depleted peridotites in both tectonic settings.","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:26287134, 研究期間(年度):2014-04-01 - 2017-03-31","subitem_description_type":"Other"},{"subitem_description":"出典：「中央海嶺下マントルの再考: マントルの均質／不均質化と海洋プレートの物質科学的実体」研究成果報告書　課題番号26287134\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-26287134/26287134seika/）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":"10.24517/00051926","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=80334746"}],"subitem_relation_type_id":{"subitem_relation_type_id_text":"https://kaken.nii.ac.jp/search/?qm=80334746","subitem_relation_type_select":"URI"}},{"subitem_relation_name":[{"subitem_relation_name_text":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-26287134/"}],"subitem_relation_type_id":{"subitem_relation_type_id_text":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-26287134/","subitem_relation_type_select":"URI"}},{"subitem_relation_name":[{"subitem_relation_name_text":"https://kaken.nii.ac.jp/report/KAKENHI-PROJECT-26287134/26287134seika/"}],"subitem_relation_type_id":{"subitem_relation_type_id_text":"https://kaken.nii.ac.jp/report/KAKENHI-PROJECT-26287134/26287134seika/","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":"2018-08-17"}],"displaytype":"detail","filename":"SC-PR-MORISHITA-T-kaken 2017-4p.pdf","filesize":[{"value":"421.7 kB"}],"format":"application/pdf","licensetype":"license_11","mimetype":"application/pdf","url":{"label":"SC-PR-MORISHITA-T-kaken 2017-4p.pdf","url":"https://kanazawa-u.repo.nii.ac.jp/record/45589/files/SC-PR-MORISHITA-T-kaken 2017-4p.pdf"},"version_id":"697854cb-c04e-40f1-8b22-46cbaa1cf8ef"}]},"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":"中央海嶺下マントルの再考: マントルの均質／不均質化と海洋プレートの物質科学的実体","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"中央海嶺下マントルの再考: マントルの均質／不均質化と海洋プレートの物質科学的実体"},{"subitem_title":"Mid-Ocean ridge peridotites revisited: homogeneity/heterogeneity and the nature of the Oceanic plate","subitem_title_language":"en"}]},"item_type_id":"9","owner":"18","path":["2817"],"pubdate":{"attribute_name":"公開日","attribute_value":"2018-08-17"},"publish_date":"2018-08-17","publish_status":"0","recid":"45589","relation_version_is_last":true,"title":["中央海嶺下マントルの再考: マントルの均質／不均質化と海洋プレートの物質科学的実体"],"weko_creator_id":"18","weko_shared_id":-1},"updated":"2023-07-27T11:23:10.715849+00:00"}