{"created":"2023-07-25T11:04:45.172209+00:00","id":7920,"links":{},"metadata":{"_buckets":{"deposit":"4ea6ca7e-561d-4b01-abb9-354ef25c9ca3"},"_deposit":{"created_by":4,"id":"7920","owners":[4],"pid":{"revision_id":0,"type":"depid","value":"7920"},"status":"published"},"_oai":{"id":"oai:nipr.repo.nii.ac.jp:00007920","sets":["1259:906:964"]},"author_link":["12538","12554"],"item_1_alternative_title_5":{"attribute_name":"論文名よみ","attribute_value_mlt":[{"subitem_alternative_title":"ナンキョク ノ カザン カツドウ ト カザンガン ノ セイシツ"}]},"item_1_biblio_info_14":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1977-03","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"234","bibliographicPageStart":"204","bibliographicVolumeNumber":"58","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":"倉沢, 一"},{"creatorName":"クラサワ, ハジメ","creatorNameLang":"ja-Kana"}],"nameIdentifiers":[{}]}]},"item_1_creator_8":{"attribute_name":"著者名(英)","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"KURASAWA, Hajime","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":"南極の火山の分布は,後期新生代に関して,いわゆる造山帯の傾向あるいは歴史と同様な特徴をもっている.南極のマリー.バードランドとビクトリアランド地域はアルカリ岩系の岩石区の特徴をもって,さまざまな変化をみせている.南極半島地域の南シェトランド諸島は玄武岩～安山岩の組み合わせで,Na成分に富むとはいうものの,それらの性質からは,アルミナに富む高アルカリソレアイト系列に属すると考えられる.ストロンチウム同位体組成などから,ロス島火山岩類は,大陸に隣接していながら,ホット・スポットという意味をもって,海洋島のそれらによくにた性質をもっているという結論がえられた.同位体地質学的あるいは化学的性質から,南極地域の火山および火山岩類を検討した.","subitem_description_type":"Other"}]},"item_1_description_12":{"attribute_name":"抄録(英)","attribute_value_mlt":[{"subitem_description":"The distribution of volcanoes in Antarctica, especially those of the later part of Cenozoic time, has considerable bearing on any interpretations of orogenic patterns or history. The volcanic rocks vary considerably in composition throughout the Marie Byrd Land and Victoria Land, forming a large alkalic province. The South Shetland Islands, lying of the Antarctic Peninsula, are composed of olivine basalt and andesite, all of which are rich in soda, but their mineralogy is similar to that of high-alkali tholeiite with high-alumina content and its derivatives. Strontium isotopes and some minor elements of the Ross Island volcanics which occur on the margin of the continent are very similar to those of oceanic island as a hot spot. In this paper the origin and differentiation of the volcanic rocks from West Antarctica are discussed on the basis of chemical composition and strontium isotopes.","subitem_description_type":"Other"}]},"item_1_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.15094/00007920","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":"Geothemical Research Section, Geological Survey of Japan"}]},"item_1_text_9":{"attribute_name":"著者所属(日)","attribute_value_mlt":[{"subitem_text_value":"通産省工業技術院地質調査所"}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"1977-03-01"}],"displaytype":"detail","filename":"KJ00002477023.pdf","filesize":[{"value":"11.5 MB"}],"format":"application/pdf","licensetype":"license_6","mimetype":"application/pdf","url":{"label":"KJ00002477023","url":"https://nipr.repo.nii.ac.jp/record/7920/files/KJ00002477023.pdf"},"version_id":"4868c387-e807-4c6d-8d26-d2c70c6fd3b1"}]},"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":"南極の火山活動と火山岩の性質","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"南極の火山活動と火山岩の性質"},{"subitem_title":"Volcanism and Volcanic Rocks in Antarctica","subitem_title_language":"en"}]},"item_type_id":"1","owner":"4","path":["964"],"pubdate":{"attribute_name":"公開日","attribute_value":"1977-03-01"},"publish_date":"1977-03-01","publish_status":"0","recid":"7920","relation_version_is_last":true,"title":["南極の火山活動と火山岩の性質"],"weko_creator_id":"4","weko_shared_id":4},"updated":"2023-07-25T11:50:44.163605+00:00"}