{"created":"2023-06-26T10:47:41.505275+00:00","id":1843,"links":{},"metadata":{"_buckets":{"deposit":"a2260a8f-61b2-4ac3-99d2-bf8748561c16"},"_deposit":{"created_by":3,"id":"1843","owners":[3],"pid":{"revision_id":0,"type":"depid","value":"1843"},"status":"published"},"_oai":{"id":"oai:sgul.repo.nii.ac.jp:00001843","sets":[]},"author_link":["2872","2873"],"item_4_alternative_title_19":{"attribute_name":"その他のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"Formation of Chemical Variation in Igneous Rocks under the Molten State : Various Parental Magmas"}]},"item_4_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2016-10-01","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"100","bibliographicPageEnd":"46","bibliographicPageStart":"13","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":"　地球の固体物質において火成岩は多くの比率を占めている。マグマの多様性は，火成岩の多様性に関わる素過程（小出，2014）におけるマグマ形成（小出，2015）の次の段階に当たる。本源マグマには，どのような多様性があり，それらがどのように生まれるのかを地質学的位置（海洋，島弧，大陸）に区分して検討した。","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":"Articles","subitem_description_type":"Other"}]},"item_4_full_name_3":{"attribute_name":"著者別名","attribute_value_mlt":[{"nameIdentifiers":[{"nameIdentifier":"2873","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":"2017-01-13"}],"displaytype":"detail","filename":"JB-100-013.pdf","filesize":[{"value":"3.3 MB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"JB-100-013.pdf","url":"https://sgul.repo.nii.ac.jp/record/1843/files/JB-100-013.pdf"},"version_id":"c1f252b6-1763-46a5-9f1e-f601c934e2c5"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"本源マグマ","subitem_subject_scheme":"Other"},{"subitem_subject":"地質学的位置","subitem_subject_scheme":"Other"},{"subitem_subject":"区分図","subitem_subject_scheme":"Other"},{"subitem_subject":"島弧","subitem_subject_scheme":"Other"},{"subitem_subject":"海洋","subitem_subject_scheme":"Other"},{"subitem_subject":"大陸","subitem_subject_scheme":"Other"},{"subitem_subject":"parental magma","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"rock series","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"geological setting","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"discrimination diagram","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"island arc","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"ocean","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"continent","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":"溶融状態における火成岩の化学的多様性の形成：多様な本源マグマ","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"溶融状態における火成岩の化学的多様性の形成：多様な本源マグマ"},{"subitem_title":"Formation of Chemical Variation in Igneous Rocks under the Molten State : Various Parental Magmas","subitem_title_language":"en"}]},"item_type_id":"4","owner":"3","path":["176"],"pubdate":{"attribute_name":"公開日","attribute_value":"2017-01-17"},"publish_date":"2017-01-17","publish_status":"0","recid":"1843","relation_version_is_last":true,"title":["溶融状態における火成岩の化学的多様性の形成：多様な本源マグマ"],"weko_creator_id":"3","weko_shared_id":3},"updated":"2023-07-26T05:42:03.528642+00:00"}