{"created":"2023-06-26T10:48:32.483432+00:00","id":2828,"links":{},"metadata":{"_buckets":{"deposit":"f4e9b17a-060a-49c3-90a8-541e253ad362"},"_deposit":{"created_by":3,"id":"2828","owners":[3],"pid":{"revision_id":0,"type":"depid","value":"2828"},"status":"published"},"_oai":{"id":"oai:sgul.repo.nii.ac.jp:00002828","sets":[]},"author_link":["4337","4336"],"item_4_alternative_title_19":{"attribute_name":"その他のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"Formation of Chemical Variations in Igneous Rocks during Consolidation Process of Magma"}]},"item_4_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2017-10-30","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"102","bibliographicPageEnd":"29","bibliographicPageStart":"1","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":"　マグマの固結過程で起こる化学的多様性形成について検討した。マグマ滞留場では，マントルから由来した玄武岩質マグマの熱によって，地殻下部の溶融により流紋岩質マグマが形成される。２つのマグマが混合することで多様なマグマ組成ができる。このようなマグマ混合作用を起こす島弧の火成作用は，大陸形成につながると考えられる。マグマだまりの冷却過程で，マグマだまりでは結晶作用，マグマ混染，液相不混和などの作用が起こる。結晶作用には平衡結晶作用と分別結晶作用があり，両者の違いで化学的多様性は大きくなる。またマグマ組成や晶出する結晶の組み合わせでも多様性が増大する。結晶作用は実測値から相図やモデル形成により推定することも可能である。噴火時には組織や構造に多様性を生じるが化学的多様性は大きくはならない。\n","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":"4337","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":"2017-11-11"}],"displaytype":"detail","filename":"JB-102-001.pdf","filesize":[{"value":"13.5 MB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"JB-102-001.pdf","url":"https://sgul.repo.nii.ac.jp/record/2828/files/JB-102-001.pdf"},"version_id":"fbb8ddd8-001d-4458-8301-0a39052538ef"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"マグマ滞留場","subitem_subject_scheme":"Other"},{"subitem_subject":"マグマだまり","subitem_subject_scheme":"Other"},{"subitem_subject":"結晶作用","subitem_subject_scheme":"Other"},{"subitem_subject":"マグマ混合","subitem_subject_scheme":"Other"},{"subitem_subject":"マグマ混染","subitem_subject_scheme":"Other"},{"subitem_subject":"液相不混和","subitem_subject_scheme":"Other"},{"subitem_subject":"magma reservoir","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"magma residence field","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"crystallization","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"magma mixing","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"magma contamination","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"magma immiscibility","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":"マグマ固結過程における火成岩の化学的多様性の形成について","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"マグマ固結過程における火成岩の化学的多様性の形成について"},{"subitem_title":"Formation of Chemical Variations in Igneous Rocks during Consolidation Process of Magma","subitem_title_language":"en"}]},"item_type_id":"4","owner":"3","path":["324"],"pubdate":{"attribute_name":"公開日","attribute_value":"2017-11-11"},"publish_date":"2017-11-11","publish_status":"0","recid":"2828","relation_version_is_last":true,"title":["マグマ固結過程における火成岩の化学的多様性の形成について"],"weko_creator_id":"3","weko_shared_id":3},"updated":"2023-07-26T05:41:27.499151+00:00"}