{"created":"2023-07-27T06:56:32.177296+00:00","id":53366,"links":{},"metadata":{"_buckets":{"deposit":"419c2d21-2c5e-4ce0-a082-214bfc4c386d"},"_deposit":{"created_by":18,"id":"53366","owners":[18],"pid":{"revision_id":0,"type":"depid","value":"53366"},"status":"published"},"_oai":{"id":"oai:kanazawa-u.repo.nii.ac.jp:00053366","sets":["2812:2813:2821"]},"author_link":["17481","2310"],"item_9_biblio_info_8":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2013-05-20","bibliographicIssueDateType":"Issued"},"bibliographicPageStart":"4p.","bibliographicVolumeNumber":"2009 – 2012","bibliographic_titles":[{"bibliographic_title":"平成24(2012)年度 科学研究費補助金 基盤研究(B) 研究成果報告書"},{"bibliographic_title":"2012 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":"本研究では,本来直接観察・サンプル採取を行えない日本列島のような島弧深部相当(最上部マントル/下部地殻)でのプロセスを理解するために,アルバニアなどに露出するオフィオライトに着目し,野外調査および,採取した試料の解析を行った。その結果, 島弧深部相当,特にマントル相当の岩相について下位から上位にかけて\n(1)中央海嶺とは異なり,流体の流入を伴うようなマグマ活動に関連した岩相が上位にかけて増加すること\n(2)かんらん岩層の上位には,シリカの付加が普遍的に観察されること\n(3)これまで中央海嶺環境で形成されて来たと考えられていた西側部分について,一部が島弧でのマグマ活動および加水作用をうけていることを明らかにした。","subitem_description_type":"Abstract"},{"subitem_description":"In order to understand the maturing processes in the deeper part of the Island arc systems, we examined arc-related ophiolites and related rocks from all over the world, particularly in the Mirdita ophiolite, Albania. Based on our filed works coupled with geochemical analyses, we concluded the maturing processes in the deeper part of the Island arc system as follows:\n(1) Effect of influx melting due to infiltration of hydrous fluids/melts are increased toward the upper section of the peridotite section, i.e., the upper most mantle section\n(2) Silica-enrichment is caused by interaction with slab-derived hydrous fluids\n(3) Peridotite massifs in the Western Mirdita Ophiolite, which had been interpreted to be of mid-ocean ridge origin, were originally formed at mid-ocean ridge setting, but was also affected by arc-related hydrous fluids/melts, resulting in the formation of fertile peridotite, such as amphibole-rich peridotites.","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:21403010, 研究期間(年度):2009 – 2012","subitem_description_type":"Other"},{"subitem_description":"出典：研究課題「島弧深部熟成過程: アルバニア・オフィオライトの地殻-マントル境界時空変動」課題番号21403010\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/ja/report/KAKENHI-PROJECT-21403010/21403010seika/）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":"10.24517/00059649","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/ja/search/?kw=80334746"}],"subitem_relation_type_id":{"subitem_relation_type_id_text":"https://kaken.nii.ac.jp/ja/search/?kw=80334746","subitem_relation_type_select":"URI"}},{"subitem_relation_name":[{"subitem_relation_name_text":"https://kaken.nii.ac.jp/ja/grant/KAKENHI-PROJECT-21403010/"}],"subitem_relation_type_id":{"subitem_relation_type_id_text":"https://kaken.nii.ac.jp/ja/grant/KAKENHI-PROJECT-21403010/","subitem_relation_type_select":"URI"}},{"subitem_relation_name":[{"subitem_relation_name_text":"https://kaken.nii.ac.jp/ja/report/KAKENHI-PROJECT-21403010/21403010seika/"}],"subitem_relation_type_id":{"subitem_relation_type_id_text":"https://kaken.nii.ac.jp/ja/report/KAKENHI-PROJECT-21403010/21403010seika/","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":"2020-11-02"}],"displaytype":"detail","filename":"SC-PR-MORISHITA-T-kaken 2013-4p.pdf","filesize":[{"value":"429.5 kB"}],"format":"application/pdf","licensetype":"license_11","mimetype":"application/pdf","url":{"label":"SC-PR-MORISHITA-T-kaken 2013-4p.pdf","url":"https://kanazawa-u.repo.nii.ac.jp/record/53366/files/SC-PR-MORISHITA-T-kaken 2013-4p.pdf"},"version_id":"ad4eb344-06b0-492d-ac7b-eb6f848dfc4b"}]},"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":"島弧深部熟成過程: アルバニア・オフィオライトの地殻-マントル境界時空変動","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"島弧深部熟成過程: アルバニア・オフィオライトの地殻-マントル境界時空変動"},{"subitem_title":"Maturing processes of deeper part of the Island arc: Diversity of crust-mantle boundary and their origins in the Albania Ophiolite","subitem_title_language":"en"}]},"item_type_id":"9","owner":"18","path":["2821"],"pubdate":{"attribute_name":"公開日","attribute_value":"2020-11-02"},"publish_date":"2020-11-02","publish_status":"0","recid":"53366","relation_version_is_last":true,"title":["島弧深部熟成過程: アルバニア・オフィオライトの地殻-マントル境界時空変動"],"weko_creator_id":"18","weko_shared_id":-1},"updated":"2023-07-27T12:07:04.988759+00:00"}