{"created":"2023-06-26T10:48:40.328469+00:00","id":2991,"links":{},"metadata":{"_buckets":{"deposit":"99b9340c-3095-44fb-97f9-ef29c9e4655a"},"_deposit":{"created_by":3,"id":"2991","owners":[3],"pid":{"revision_id":0,"type":"depid","value":"2991"},"status":"published"},"_oai":{"id":"oai:sgul.repo.nii.ac.jp:00002991","sets":[]},"author_link":["553","552"],"item_4_alternative_title_19":{"attribute_name":"その他のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"Geological Significances of Island Arcs on Orogeny"}]},"item_4_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2019-10-31","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"106","bibliographicPageEnd":"61","bibliographicPageStart":"27","bibliographic_titles":[{"bibliographic_title":"札幌学院大学人文学会紀要 = Journal of the Society of Humanities"}]}]},"item_4_description_4":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"　造山運動はテクトニクスの一面だと位置づけられる。造山運動は地球でもっとも大規模な地質学的に活発な営みとなる。造山運動は，衝突型と太平洋型に分けられ，太平洋型は沈み込み帯で形成される。沈み込み帯では，構造浸食作用も働くことから，造山帯の形成には至らないものも多い。激しい太平洋型造山運動が起こるのは，海嶺の沈み込みの時期の島弧形成だと考えられるようになってきた。","subitem_description_type":"Abstract"},{"subitem_description":"　Orogeny is a part of the tectonics, and is most active geological functions on the Earth. Orogeny is classified with the collision-type and the Pacific-type. The Pacific-type orogeny is developed at subduction zone, but orogeny belt often is not developed by structure erosion at a subduction zone. The intense Pacific-type orogeny is formed at the island arc subducted by oceanic ridge, for example, Southwest Japan arc.","subitem_description_type":"Abstract"}]},"item_4_description_40":{"attribute_name":"資源タイプ","attribute_value_mlt":[{"subitem_description":"Bulletin","subitem_description_type":"Other"}]},"item_4_description_5":{"attribute_name":"内容記述","attribute_value_mlt":[{"subitem_description":"論文","subitem_description_type":"Other"},{"subitem_description":"Article","subitem_description_type":"Other"}]},"item_4_full_name_3":{"attribute_name":"著者別名","attribute_value_mlt":[{"nameIdentifiers":[{"nameIdentifier":"553","nameIdentifierScheme":"WEKO"}],"names":[{"name":"KOIDE, Yoshiyuki"}]}]},"item_4_publisher_33":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"札幌学院大学総合研究所 = Research Institute of Sapporo Gakuin University"}]},"item_4_source_id_8":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"0916-3166","subitem_source_identifier_type":"ISSN"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"小出, 良幸"}],"nameIdentifiers":[{}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2019-11-15"}],"displaytype":"detail","filename":"JB-106-027.pdf","filesize":[{"value":"2.3 MB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"JB-106-027.pdf","url":"https://sgul.repo.nii.ac.jp/record/2991/files/JB-106-027.pdf"},"version_id":"16bea258-c4ce-494a-a8b8-e76bed2ecf40"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"太平洋型造山運動","subitem_subject_scheme":"Other"},{"subitem_subject":"構造侵食作用","subitem_subject_scheme":"Other"},{"subitem_subject":"低温高圧型変成岩","subitem_subject_scheme":"Other"},{"subitem_subject":"TTG","subitem_subject_scheme":"Other"},{"subitem_subject":"テクトニクス","subitem_subject_scheme":"Other"},{"subitem_subject":"Pacific-type orogeny","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"tectonic erosion","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"low-pressure and high-temperature metamorphic rock","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"TTG","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"tectonics","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":"造山運動からみた島弧の地質学的位置づけ","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"造山運動からみた島弧の地質学的位置づけ"},{"subitem_title":"Geological Significances of Island Arcs on Orogeny","subitem_title_language":"en"}]},"item_type_id":"4","owner":"3","path":["344"],"pubdate":{"attribute_name":"公開日","attribute_value":"2019-11-15"},"publish_date":"2019-11-15","publish_status":"0","recid":"2991","relation_version_is_last":true,"title":["造山運動からみた島弧の地質学的位置づけ"],"weko_creator_id":"3","weko_shared_id":3},"updated":"2023-07-26T05:39:09.963380+00:00"}