{"created":"2023-07-27T06:52:14.210354+00:00","id":46028,"links":{},"metadata":{"_buckets":{"deposit":"88f8cf0d-cec6-4811-bfc1-bfa20b911cfa"},"_deposit":{"created_by":18,"id":"46028","owners":[18],"pid":{"revision_id":0,"type":"depid","value":"46028"},"status":"published"},"_oai":{"id":"oai:kanazawa-u.repo.nii.ac.jp:00046028","sets":["2812:2813:2818"]},"author_link":["79877","2446"],"item_9_biblio_info_8":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2016-06-13","bibliographicIssueDateType":"Issued"},"bibliographicPageStart":"6p.","bibliographicVolumeNumber":"2013-04-01 - 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(C) 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":"オマーンオフィオライトのV3溶岩原は少なくとも上下2枚の溶岩流からなり，基本的な構造は陸上の洪水玄武岩に類似し，塊状コアが上下の柱状節理の発達したクラストに挟在する。V3溶岩は噴出初期に未分化な溶岩を流出し，クライマックスに分化した溶岩を流出し，噴火末期にかけて再び未分化な溶岩を噴出した。供給岩脈から6.0 km地点の層序方向の下部溶岩流の組成変化は内成的な成長で説明できる。一方，上部溶岩は順次溶岩ローブが累積・溶結して形成された。","subitem_description_type":"Abstract"},{"subitem_description":"The V3 Volcanic rocks of the Oman Ophiolite are thick submarine lava flows exceeding an estimated volume of several cubic kilometers. The V3 flow field consists of massive cores sandwiched between columnar jointed lava crusts. The V3 flow is divided into the Upper and the Lower flow by the intervening pillow lava and shale. Yb variation of the lower flow is consistent with the internal growth of inflating sheet where newly supplied lava was injected into the core of the flow, whereas the upper flow was empalced lobe by lobe one after the top of the other, which were welded togher to form a massive sheet-like lava.","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:25400446, 研究期間(年度):2013-04-01 - 2016-03-31","subitem_description_type":"Other"},{"subitem_description":"出典：研究課題「巨大海底溶岩流の定置過程の解明」課題番号:25400446\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-25400446/25400446seika/）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":"10.24517/00052362","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=30192511"}],"subitem_relation_type_id":{"subitem_relation_type_id_text":"https://kaken.nii.ac.jp/search/?qm=30192511","subitem_relation_type_select":"URI"}},{"subitem_relation_name":[{"subitem_relation_name_text":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-25400446/"}],"subitem_relation_type_id":{"subitem_relation_type_id_text":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-25400446/","subitem_relation_type_select":"URI"}},{"subitem_relation_name":[{"subitem_relation_name_text":"https://kaken.nii.ac.jp/report/KAKENHI-PROJECT-25400446/25400446seika/"}],"subitem_relation_type_id":{"subitem_relation_type_id_text":"https://kaken.nii.ac.jp/report/KAKENHI-PROJECT-25400446/25400446seika/","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":"2018-09-28"}],"displaytype":"detail","filename":"SC-PR-UMINO-S-kaken 2016-6p.pdf","filesize":[{"value":"1.1 MB"}],"format":"application/pdf","licensetype":"license_11","mimetype":"application/pdf","url":{"label":"SC-PR-UMINO-S-kaken 2016-6p.pdf","url":"https://kanazawa-u.repo.nii.ac.jp/record/46028/files/SC-PR-UMINO-S-kaken 2016-6p.pdf"},"version_id":"7a8b737d-8632-476f-867a-fc4cace0e803"}]},"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":"巨大海底溶岩流の定置過程の解明","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"巨大海底溶岩流の定置過程の解明"},{"subitem_title":"Emplacement proceses of large submarine lava flows","subitem_title_language":"en"}]},"item_type_id":"9","owner":"18","path":["2818"],"pubdate":{"attribute_name":"公開日","attribute_value":"2018-10-04"},"publish_date":"2018-10-04","publish_status":"0","recid":"46028","relation_version_is_last":true,"title":["巨大海底溶岩流の定置過程の解明"],"weko_creator_id":"18","weko_shared_id":-1},"updated":"2023-07-27T10:48:00.526167+00:00"}