{"created":"2023-07-25T11:04:00.464984+00:00","id":7008,"links":{},"metadata":{"_buckets":{"deposit":"65f67599-4201-4ad6-b0c5-73212efb0074"},"_deposit":{"created_by":4,"id":"7008","owners":[4],"pid":{"revision_id":0,"type":"depid","value":"7008"},"status":"published"},"_oai":{"id":"oai:nipr.repo.nii.ac.jp:00007008","sets":["1259:906:917"]},"author_link":["10707","10703","10704","10708"],"item_1_alternative_title_5":{"attribute_name":"論文名よみ","attribute_value_mlt":[{"subitem_alternative_title":"ショウワキチ サン ホウシャセイ コウブツ Euxenite-Polycrase ケイ コウブツ ニ ツイテ"}]},"item_1_biblio_info_14":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1961-01","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"750","bibliographicPageStart":"747","bibliographicVolumeNumber":"11","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":"林, 昇一郎"},{"creatorName":"ハヤシ, ショウイチロウ","creatorNameLang":"ja-Kana"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"長島, 弘三"},{"creatorName":"ナガシマ, コウゾウ","creatorNameLang":"ja-Kana"}],"nameIdentifiers":[{}]}]},"item_1_creator_8":{"attribute_name":"著者名(英)","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"HAYASHI, Shoichiro","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"NAGASHIMA, Kozo","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":"本鉱物は黒色塊状,貝殻状断口,ガラス光沢を示し,比重は約5.5である.条痕は赤褐色で,千度加熱後は淡褐色に変ずる.薄片の色は赤褐色,等方性を示す.粉末のガイガー計数器による放射能は約15%U当量である.常温ではX線粉末像が得られず,完全にメタミクト状態にある.空気中で1,000℃ 7 時間加熱した試料のX線粉末像は,euxeniteの標準資料とよく一致する.DTA曲線は約760℃に著しい発熱があり,euxenite, eschyniteの特徴を示す.主要化学成分(%)はU0_2 11.84, U0_3 0.67, Th0_2 3.20, Ti0_2 24.74, Nb_20_5+Ta_20_5 30.76,ΣCe_20_3 0.38,ΣΥ_20_3 25.26などでAB_20_6の理想式で表わされる.Nb_20_5とTa_20_5の量は略等量であり(Nb_20_5+Ta_20_5):Ti0_2の分子比は1:3.6になり,化学成分上からはBROGGERの定義によるpolyeraseに属するものである.","subitem_description_type":"Other"}]},"item_1_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.15094/00007008","subitem_identifier_reg_type":"JaLC"}]},"item_1_publisher_22":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"国立極地研究所"}]},"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":"551.1/.4:552","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":"Geological Survey of Japan"},{"subitem_text_language":"en","subitem_text_value":"Chemical Institute, College of General Education, University of Tokyo"}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"1961-01-01"}],"displaytype":"detail","filename":"KJ00002406672.pdf","filesize":[{"value":"438.1 kB"}],"format":"application/pdf","licensetype":"license_6","mimetype":"application/pdf","url":{"label":"KJ00002406672","url":"https://nipr.repo.nii.ac.jp/record/7008/files/KJ00002406672.pdf"},"version_id":"5577ec3d-aad6-4d10-94d8-bd922fed06c6"}]},"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":"昭和基地産放射性鉱物-Euxenite-Polycrase系鉱物-について(地学部門)(<特集>南極シンポジウム)","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"昭和基地産放射性鉱物-Euxenite-Polycrase系鉱物-について(地学部門)(<特集>南極シンポジウム)"},{"subitem_title":"A Mineralogical Note on the Euxenite-Polycrase Series Mineral from Syowa Base, Antarctica (EARTH SCIENCE) (<Special Publication>Antarctic Symposium in Tokyo, 1960)","subitem_title_language":"en"}]},"item_type_id":"1","owner":"4","path":["917"],"pubdate":{"attribute_name":"公開日","attribute_value":"1961-01-01"},"publish_date":"1961-01-01","publish_status":"0","recid":"7008","relation_version_is_last":true,"title":["昭和基地産放射性鉱物-Euxenite-Polycrase系鉱物-について(地学部門)(<特集>南極シンポジウム)"],"weko_creator_id":"4","weko_shared_id":4},"updated":"2023-07-25T11:59:24.013906+00:00"}