{"created":"2023-07-25T11:05:07.245415+00:00","id":8363,"links":{},"metadata":{"_buckets":{"deposit":"1e5ecd3d-3b48-47ea-bf54-b566163d9f78"},"_deposit":{"created_by":4,"id":"8363","owners":[4],"pid":{"revision_id":0,"type":"depid","value":"8363"},"status":"published"},"_oai":{"id":"oai:nipr.repo.nii.ac.jp:00008363","sets":["1259:906:985"]},"author_link":["41","10931","447","14670"],"item_1_alternative_title_5":{"attribute_name":"論文名よみ","attribute_value_mlt":[{"subitem_alternative_title":"ナンキョク インセキ ALH-77219 メソシデライト ノ ジキ ブンセキ"}]},"item_1_biblio_info_14":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1983-09","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"10","bibliographicPageStart":"1","bibliographicVolumeNumber":"79","bibliographic_titles":[{"bibliographic_title":"南極資料"}]}]},"item_1_creator_6":{"attribute_name":"著者名(日)","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"永田, 武"},{"creatorName":"ナガタ, タケシ","creatorNameLang":"ja-Kana"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"船木, 實"},{"creatorName":"フナキ, ミノル","creatorNameLang":"ja-Kana"}],"nameIdentifiers":[{}]}]},"item_1_creator_8":{"attribute_name":"著者名(英)","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"Nagata, Takesi","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Funaki, Minoru","creatorNameLang":"en"}],"nameIdentifiers":[{}]}]},"item_1_description_1":{"attribute_name":"ページ属性","attribute_value_mlt":[{"subitem_description":"P(論文)","subitem_description_type":"Other"}]},"item_1_description_11":{"attribute_name":"抄録(日)","attribute_value_mlt":[{"subitem_description":"南極隕石のコレクションのうちでは稀少な, メソシデライトALH-77219の磁気分析を行い, また, その中に含まれる金属粒の化学成分について, EPMAによる分析を行った。EPMA分析の結果, ALH-77219中の金属相は, Ni含有量5-6wt%のカマサイトおよびNi含有量約50wt%のテーナイト相とに2分される。ALH-77219の熱磁化曲線は, 平均Ni含有量6wt%のカマサイトと平均Ni含有量54wt%のテーナイトが混在し, そのテーナイト相の大部分は, テトラテーナイト規則格子構造を持つことを示す。6% Niカマサイトおよび54% Niテーナイトの含有量は, それぞれ19.3wt%および6.3wt%である。","subitem_description_type":"Other"}]},"item_1_description_12":{"attribute_name":"抄録(英)","attribute_value_mlt":[{"subitem_description":"Magnetic analyses are made on an Antarctic mesosiderite ALH-77219,and chemical analyses of metallic grains in the mesosiderite are carried out with the aid of an EPMA. The EPMA analyses show that the metallic phases in ALH-77219 are composed of kamacite of 5-6wt% Ni and taenite of about 50wt% Ni. The thermomagnetic analyses show that the mesosiderite ALH-77219 contains kamacite phase of about 6wt% Ni on average of 19.3% in weight and taenite phase of about 54wt% Ni on average of 6.3% in weight. The major parts of the taenite phase are of the superlattice structure of tetrataenite, which has a large magnetic anisotropy.","subitem_description_type":"Other"}]},"item_1_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.15094/00008363","subitem_identifier_reg_type":"JaLC"}]},"item_1_source_id_13":{"attribute_name":"雑誌書誌ID","attribute_value_mlt":[{"subitem_source_identifier":"AN00181831","subitem_source_identifier_type":"NCID"}]},"item_1_source_id_20":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"00857289","subitem_source_identifier_type":"ISSN"}]},"item_1_subject_21":{"attribute_name":"国際十進分類法","attribute_value_mlt":[{"subitem_subject":"552.6","subitem_subject_scheme":"UDC"}]},"item_1_text_10":{"attribute_name":"著者所属(英)","attribute_value_mlt":[{"subitem_text_language":"en","subitem_text_value":"National Institute of Polar Research"},{"subitem_text_language":"en","subitem_text_value":"National Institute of Polar Research"}]},"item_1_text_9":{"attribute_name":"著者所属(日)","attribute_value_mlt":[{"subitem_text_value":"国立極地研究所"},{"subitem_text_value":"国立極地研究所"}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"1983-09-01"}],"displaytype":"detail","filename":"KJ00000139577.pdf","filesize":[{"value":"795.4 kB"}],"format":"application/pdf","licensetype":"license_6","mimetype":"application/pdf","url":{"label":"KJ00000139577","url":"https://nipr.repo.nii.ac.jp/record/8363/files/KJ00000139577.pdf"},"version_id":"1aed31bc-7f76-4a08-89e3-f23460dd0156"}]},"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":"departmental bulletin paper","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_title":"南極隕石ALH-77219メソシデライトの磁気分析","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"南極隕石ALH-77219メソシデライトの磁気分析"},{"subitem_title":"Magnetic analysis of an Antarctic mesosiderite, ALH-77219","subitem_title_language":"en"}]},"item_type_id":"1","owner":"4","path":["985"],"pubdate":{"attribute_name":"公開日","attribute_value":"1983-09-01"},"publish_date":"1983-09-01","publish_status":"0","recid":"8363","relation_version_is_last":true,"title":["南極隕石ALH-77219メソシデライトの磁気分析"],"weko_creator_id":"4","weko_shared_id":4},"updated":"2023-07-25T13:31:24.241328+00:00"}