{"created":"2023-06-19T09:11:03.007123+00:00","id":22667,"links":{},"metadata":{"_buckets":{"deposit":"af9858c9-e784-4312-b0ff-3ea586667625"},"_deposit":{"created_by":1,"id":"22667","owners":[1],"pid":{"revision_id":0,"type":"depid","value":"22667"},"status":"published"},"_oai":{"id":"oai:kumadai.repo.nii.ac.jp:00022667","sets":["448:449"]},"author_link":["98534","98540","98531","98530","98533","98538","98543","98541","98542","98529","98535","98539","98528","98536","98537","98532"],"item_17_biblio_info_6":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2007","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"237","bibliographicPageStart":"235","bibliographicVolumeNumber":"882","bibliographic_titles":[{"bibliographic_title":"AIP Conference Proceedings"}]}]},"item_17_creator_3":{"attribute_name":"別言語の著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"古川, 由紀"}],"nameIdentifiers":[{"nameIdentifier":"98540","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"吉朝, 朗"}],"nameIdentifiers":[{"nameIdentifier":"98541","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"奥部, 真樹"}],"nameIdentifiers":[{"nameIdentifier":"98542","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"西山, 忠男"}],"nameIdentifiers":[{"nameIdentifier":"98543","nameIdentifierScheme":"WEKO"}]}]},"item_17_description_17":{"attribute_name":"フォーマット","attribute_value_mlt":[{"subitem_description":"application/pdf","subitem_description_type":"Other"}]},"item_17_description_46":{"attribute_name":"資源タイプ","attribute_value_mlt":[{"subitem_description":"論文(Article)","subitem_description_type":"Other"}]},"item_17_description_5":{"attribute_name":"内容記述","attribute_value_mlt":[{"subitem_description":"We measured XAFS spectra near the Ti, V, Cr, Mn, Fe, Co, Ni, Cu and Zn K-edges in Al2SiO5 polymorphs to reveal the local structure around these elements in the minerals. XANES spectra show that the valence of Fe and Cr is different depending on the crystal structure and formation environments. The spectra of kyanite, a high pressure mineral, shift to high energy side. The Fe-O bond length of kyanite determined by EXAFS data analyses is the shortest of all samples.","subitem_description_type":"Other"}]},"item_17_description_77":{"attribute_name":"URL","attribute_value_mlt":[{"subitem_description":"http://proceedings.aip.org/proceedings/","subitem_description_type":"Other"}]},"item_17_publisher_36":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"American Institute of 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課題番号:17204049『微量元素の局所構造に残された惑星地球活動の重要情報の解読』に掲載"}]},"item_17_version_type_19":{"attribute_name":"著者版フラグ","attribute_value_mlt":[{"subitem_version_type":"VoR"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"Furukawa, Yuki"}],"nameIdentifiers":[{"nameIdentifier":"98528","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"Yoshiasa, Akira"}],"nameIdentifiers":[{"nameIdentifier":"98529","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"Arima, Hiroshi"}],"nameIdentifiers":[{"nameIdentifier":"98530","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"Okube, Maki"}],"nameIdentifiers":[{"nameIdentifier":"98531","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"Murai, Keiichiro"}],"nameIdentifiers":[{"nameIdentifier":"98532","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"Nishiyama, Tadao"}],"nameIdentifiers":[{"nameIdentifier":"98533","nameIdentifierScheme":"WEKO"}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2020-03-02"}],"displaytype":"detail","filename":"AIP2007_235-237.pdf","filesize":[{"value":"437.8 kB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"AIP2007_235-237.pdf","url":"https://kumadai.repo.nii.ac.jp/record/22667/files/AIP2007_235-237.pdf"},"version_id":"1558b1f3-c5c4-400a-977e-8c6d4b153adc"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"Andalusite","subitem_subject_scheme":"Other"},{"subitem_subject":"sillimanite","subitem_subject_scheme":"Other"},{"subitem_subject":"Kyanite","subitem_subject_scheme":"Other"},{"subitem_subject":"Transition element","subitem_subject_scheme":"Other"},{"subitem_subject":"Mineral","subitem_subject_scheme":"Other"},{"subitem_subject":"XAFS","subitem_subject_scheme":"Other"}]},"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":"conference paper","resourceuri":"http://purl.org/coar/resource_type/c_5794"}]},"item_title":"Local structure of transition elements (V, Cr, Mn, Fe and Zn) in Al2SiO5 polymorphs","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"Local structure of transition elements (V, Cr, Mn, Fe and Zn) in Al2SiO5 polymorphs"}]},"item_type_id":"17","owner":"1","path":["449"],"pubdate":{"attribute_name":"公開日","attribute_value":"2009-09-24"},"publish_date":"2009-09-24","publish_status":"0","recid":"22667","relation_version_is_last":true,"title":["Local structure of transition elements (V, Cr, Mn, Fe and Zn) in Al2SiO5 polymorphs"],"weko_creator_id":"1","weko_shared_id":-1},"updated":"2023-06-19T18:49:37.934251+00:00"}