{"created":"2023-05-15T14:37:34.922732+00:00","id":48480,"links":{},"metadata":{"_buckets":{"deposit":"7fd5f77e-2603-48b5-b926-37275715d47a"},"_deposit":{"created_by":1,"id":"48480","owners":[1],"pid":{"revision_id":0,"type":"depid","value":"48480"},"status":"published"},"_oai":{"id":"oai:repo.qst.go.jp:00048480","sets":["1"]},"author_link":["487400","487401","487404","487402","487406","487399","487405","487403","487398"],"item_8_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2017-12","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"10","bibliographicPageEnd":"2112","bibliographicPageStart":"2106","bibliographicVolumeNumber":"102","bibliographic_titles":[{"bibliographic_title":"American Mineralogist"}]}]},"item_8_description_5":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"本研究は、QST専用ビームラインBL11XUにおいて地球深部のマグマ類似体である玄武岩ガラス中の鉄のスピン状態と電子環境を高圧下放射光メスバウアー分光法で調べた研究報告である。スペクトル解析で定量的に求めたFe3+/ΣFe値の圧力依存性から、玄武岩ガラス中のFeの高スピンFe2+、高スピンFe3+の比率は130 GPaの地球深部高圧下まで維持されることが分かった。この実験からは、玄武岩ガラスではFeのスピンクロスオーバ転移（高スピンFe2+ →低スピンFe2+）が起きないことも明らかになった。これら結果は、地球深部のマグマの物性を理解する上での有用な知見となる。","subitem_description_type":"Abstract"}]},"item_8_relation_14":{"attribute_name":"DOI","attribute_value_mlt":[{"subitem_relation_type_id":{"subitem_relation_type_id_text":"10.2138/am-2017-6035","subitem_relation_type_select":"DOI"}}]},"item_access_right":{"attribute_name":"アクセス権","attribute_value_mlt":[{"subitem_access_right":"metadata only access","subitem_access_right_uri":"http://purl.org/coar/access_right/c_14cb"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"Maeda, Fumiya"}],"nameIdentifiers":[{"nameIdentifier":"487398","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"Kamad, Seiji"}],"nameIdentifiers":[{"nameIdentifier":"487399","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"Ohtani, Eiji"}],"nameIdentifiers":[{"nameIdentifier":"487400","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"McCammon, Catherine"}],"nameIdentifiers":[{"nameIdentifier":"487401","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"Miyahara, Masaaki"}],"nameIdentifiers":[{"nameIdentifier":"487402","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"Masuda, Ryo"}],"nameIdentifiers":[{"nameIdentifier":"487403","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"Mitsui, Takaya"}],"nameIdentifiers":[{"nameIdentifier":"487404","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"Hirao, Naohisa"}],"nameIdentifiers":[{"nameIdentifier":"487405","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"三井 隆也","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"487406","nameIdentifierScheme":"WEKO"}]}]},"item_language":{"attribute_name":"言語","attribute_value_mlt":[{"subitem_language":"eng"}]},"item_resource_type":{"attribute_name":"資源タイプ","attribute_value_mlt":[{"resourcetype":"journal article","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_title":"Spin state and electronic environment of iron in basaltic glass in the lower mantle","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"Spin state and electronic environment of iron in basaltic glass in the lower mantle"}]},"item_type_id":"8","owner":"1","path":["1"],"pubdate":{"attribute_name":"公開日","attribute_value":"2018-02-08"},"publish_date":"2018-02-08","publish_status":"0","recid":"48480","relation_version_is_last":true,"title":["Spin state and electronic environment of iron in basaltic glass in the lower mantle"],"weko_creator_id":"1","weko_shared_id":-1},"updated":"2023-05-15T23:27:35.524798+00:00"}