{"created":"2023-07-25T11:04:58.504612+00:00","id":8184,"links":{},"metadata":{"_buckets":{"deposit":"65ca0d3c-c9f1-47ac-ba66-f429fa3ab7bc"},"_deposit":{"created_by":4,"id":"8184","owners":[4],"pid":{"revision_id":0,"type":"depid","value":"8184"},"status":"published"},"_oai":{"id":"oai:nipr.repo.nii.ac.jp:00008184","sets":["1259:906:976"]},"author_link":["14306","14302","12839","435"],"item_1_alternative_title_5":{"attribute_name":"論文名よみ","attribute_value_mlt":[{"subitem_alternative_title":"ヤマト サンミャク ト ショウワ キチ シュウヘンサン ガンセキ ノ U Th K セイブン ノ ヨサツ"}]},"item_1_biblio_info_14":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1980-09","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"30","bibliographicPageStart":"25","bibliographicVolumeNumber":"70","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":"白石, 和行"},{"creatorName":"シライシ, カズユキ","creatorNameLang":"ja-Kana"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"金谷, 弘"},{"creatorName":"カナヤ, ヒロシ","creatorNameLang":"ja-Kana"}],"nameIdentifiers":[{}]}]},"item_1_creator_8":{"attribute_name":"著者名(英)","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"SHIRAISHI, Kazuyuki","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"KANAYA, Hiroshi","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":"やまと山脈と昭和基地周辺の12個の岩石のウラン,トリウムおよびカリウム含有量を,ガンマ線スペクトロメトリー法によって測定した.塩基性-超塩基性変成岩は3成分とも,きわめて低い含有量を示すが,花崗岩質岩は幅広い変化を示す.各成分の量比を,本邦産の花崗岩質岩と比較した.","subitem_description_type":"Other"}]},"item_1_description_12":{"attribute_name":"抄録(英)","attribute_value_mlt":[{"subitem_description":"Uranium, thorium and potassium contents of the twelve rocks from the Yamato Mountains and the vicinity of Syowa Station were quantitatively analysed by γ spectrometry method. Basic to ultrabasic metamorphic rocks have remarkably low contents of these elements. On the other hand, granitic rocks show variable contents. The ratios of these elements were examined in comparison with those of granitic rocks in Japan.","subitem_description_type":"Other"}]},"item_1_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.15094/00008184","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":"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":"National Institute of Polar Research"},{"subitem_text_language":"en","subitem_text_value":"Geological Survey of Japan"}]},"item_1_text_2":{"attribute_name":"記事種別(日)","attribute_value_mlt":[{"subitem_text_value":"研究論文"}]},"item_1_text_3":{"attribute_name":"記事種別(英)","attribute_value_mlt":[{"subitem_text_language":"en","subitem_text_value":"Scientific Paper"}]},"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":"地質調査所"}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"1980-09-01"}],"displaytype":"detail","filename":"KJ00002477244.pdf","filesize":[{"value":"2.0 MB"}],"format":"application/pdf","licensetype":"license_6","mimetype":"application/pdf","url":{"label":"KJ00002477244","url":"https://nipr.repo.nii.ac.jp/record/8184/files/KJ00002477244.pdf"},"version_id":"128a50c6-a2aa-4072-a4fb-547b9f72ebf2"}]},"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":"やまと山脈と昭和基地周辺産岩石のU,Th,K成分の予察","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"やまと山脈と昭和基地周辺産岩石のU,Th,K成分の予察"},{"subitem_title":"Preliminary Note on U, Th and K Contents of Some Rocks from the Yamato Mountains and the Vicinity of Syowa Station, East Antarctica","subitem_title_language":"en"}]},"item_type_id":"1","owner":"4","path":["976"],"pubdate":{"attribute_name":"公開日","attribute_value":"1980-09-01"},"publish_date":"1980-09-01","publish_status":"0","recid":"8184","relation_version_is_last":true,"title":["やまと山脈と昭和基地周辺産岩石のU,Th,K成分の予察"],"weko_creator_id":"4","weko_shared_id":4},"updated":"2023-07-25T13:30:22.017298+00:00"}