{"created":"2023-07-25T11:01:11.718191+00:00","id":3125,"links":{},"metadata":{"_buckets":{"deposit":"39233e8b-2e4d-4d9f-8339-6c9ecba9d27c"},"_deposit":{"created_by":4,"id":"3125","owners":[4],"pid":{"revision_id":0,"type":"depid","value":"3125"},"status":"published"},"_oai":{"id":"oai:nipr.repo.nii.ac.jp:00003125","sets":["1259:1260:1265:435:441"]},"author_link":["65715","716","65714","65713","1896","17217"],"item_1_biblio_info_14":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2003-10","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"136","bibliographicPageStart":"108","bibliographicVolumeNumber":"16","bibliographic_titles":[{"bibliographic_title":"Polar geoscience"}]}]},"item_1_creator_8":{"attribute_name":"著者名(英)","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"Owada, Masaaki","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Baba, Sotaro","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Laufer, Andreas L.","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Elvevold, Synnoeve","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Shiraishi, Kazuyuki","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Jacobs, Joachim","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_12":{"attribute_name":"抄録(英)","attribute_value_mlt":[{"subitem_description":"The geological history of Filchnerfjella and surrounding areas (2゜E to 8゜E) in central Dronning Maud Land,East Antarctica,is constructed from metamorphic and igneous petrology,and structural investigations.The geology of Filchner-fjella consists mainly of metamorphic rocks accompanied by intrusive rocks.Two stages of metamorphism can be recognized in this area.The earlier stage metamorphism is defined as a porphyroblast stage (garnet,hornblende,and sillimanite stable), and the later one is recognized as a symplectic stage (orthopyroxene and cordieritestable).Taking metamorphic textures and geothermobarometries into account,the rocks experienced an early high-P/medium-T followed by a low-P and high-T stage. Partial melting took place during the low-P/high-T stage,because probable melt of leucocratic gneiss contains cordierite.The field relationships and petrography of the syenite at Filchnerfjella are similar to those of post-tectonic plutons from central Dronning Maud Land,and most of the post-tectonic intrusive rocks have within-plate geochemical features.The structural history in Filchnerfjella and surrounding areas can be divided into the Pan-African stage and the Meso to Cenozoic stage that relates to the break-up of Gondwana.","subitem_description_type":"Other"}]},"item_1_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.15094/00003125","subitem_identifier_reg_type":"JaLC"}]},"item_1_publisher_22":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"National Institute of Polar Research"}]},"item_1_source_id_13":{"attribute_name":"雑誌書誌ID","attribute_value_mlt":[{"subitem_source_identifier":"AA1130866X","subitem_source_identifier_type":"NCID"}]},"item_1_text_10":{"attribute_name":"著者所属(英)","attribute_value_mlt":[{"subitem_text_language":"en","subitem_text_value":"Department of Earth Sciences, Yamaguchi University/Department of Natural Environment, University of the Ryukyus/Geologisch-Palaontologisches Institut, Johann Wolfgang Goethe-Universitat/Norwegian Polar Institute/National Institute of Polar Research/Universitat Bremen"}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2003-10-01"}],"displaytype":"detail","filename":"KJ00000044119.pdf","filesize":[{"value":"5.4 MB"}],"format":"application/pdf","licensetype":"license_6","mimetype":"application/pdf","url":{"label":"KJ00000044119","url":"https://nipr.repo.nii.ac.jp/record/3125/files/KJ00000044119.pdf"},"version_id":"fd3f57be-6270-4af2-8248-ea105bd1aa03"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"central Dronning Maud Land","subitem_subject_scheme":"Other"},{"subitem_subject":"geology of Filchnerfjella","subitem_subject_scheme":"Other"},{"subitem_subject":"two-stage meta-morphism","subitem_subject_scheme":"Other"},{"subitem_subject":"Pan-African magmatism","subitem_subject_scheme":"Other"},{"subitem_subject":"Gondwana break-up","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":"departmental bulletin paper","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_title":"Geology of eastern Muhlig -Hofmannfjella and Filchnerfjella in Dronning Maud Land, East Antarctica; A preliminary report of a Japan-Norway-Germany joint geological investigation","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"Geology of eastern Muhlig -Hofmannfjella and Filchnerfjella in Dronning Maud Land, East Antarctica; A preliminary report of a Japan-Norway-Germany joint geological investigation"}]},"item_type_id":"1","owner":"4","path":["441"],"pubdate":{"attribute_name":"公開日","attribute_value":"2003-10-01"},"publish_date":"2003-10-01","publish_status":"0","recid":"3125","relation_version_is_last":true,"title":["Geology of eastern Muhlig -Hofmannfjella and Filchnerfjella in Dronning Maud Land, East Antarctica; A preliminary report of a Japan-Norway-Germany joint geological investigation"],"weko_creator_id":"4","weko_shared_id":4},"updated":"2023-07-25T12:34:43.504905+00:00"}