{"created":"2023-07-25T11:00:33.906694+00:00","id":2414,"links":{},"metadata":{"_buckets":{"deposit":"12698eb6-172e-49b3-b810-89e6a0169b50"},"_deposit":{"created_by":4,"id":"2414","owners":[4],"pid":{"revision_id":0,"type":"depid","value":"2414"},"status":"published"},"_oai":{"id":"oai:nipr.repo.nii.ac.jp:00002414","sets":["1:356:409"]},"author_link":["55939","55940","1961","55938"],"item_1_biblio_info_14":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2001-07","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"86","bibliographicPageStart":"59","bibliographicVolumeNumber":"55","bibliographic_titles":[{"bibliographic_title":"Memoirs of National Institute of Polar Research. Special issue"}]}]},"item_1_creator_8":{"attribute_name":"著者名(英)","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"Grantham,G.H.","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Eglington,B.M.","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Thomas, R.J.","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Mendonidis, P.","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 ∿1030-1090Ma old, locally charnockitic, intrusions which are exposed from Namaqualand in the west, through Natal, into the Maud Province Antarctica in the east, show A-type, within plate granite characteristics. The major and trace element characteristics from all the intrusions are remarkably similar and consistent and are typical of C-Type charnockites. Two-pyroxene thermometry as well as thermometry utilising calibrations from experimental studies of saturation surfaces using Zr, P and Ti suggest temperatures between ∿850℃ and ∿1100℃. Pressure estimates from aureole assemblages suggest depths of emplacement between 30-10km. Available isotopic data suggest magma sources in Natal and Antarctica were juvenile, probably mantle derived whereas those in Namaqualand suggest a significant crustal contribution.","subitem_description_type":"Other"}]},"item_1_source_id_13":{"attribute_name":"雑誌書誌ID","attribute_value_mlt":[{"subitem_source_identifier":"AA00733561","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":"Council for Geoscience/Council for Geoscience/Council for Geoscience/Department of Metallurgy, Vaal Triangle Technikon"}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2001-07-01"}],"displaytype":"detail","filename":"KJ00000012966.pdf","filesize":[{"value":"3.0 MB"}],"format":"application/pdf","licensetype":"license_6","mimetype":"application/pdf","url":{"label":"KJ00000012966","url":"https://nipr.repo.nii.ac.jp/record/2414/files/KJ00000012966.pdf"},"version_id":"6abcb228-a992-4e85-83db-b20dd6316c1d"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"charnockite","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"A-type","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"Natal","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"Namaqualand","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"Dronning Maud Land","subitem_subject_language":"en","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":"The nature of the Grenville-age charnockitic A-type magmatism from the Natal, Namaqua and Maud Belts of southern Africa and western Dronning Maud Land, Antarctica","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"The nature of the Grenville-age charnockitic A-type magmatism from the Natal, Namaqua and Maud Belts of southern Africa and western Dronning Maud Land, Antarctica","subitem_title_language":"en"}]},"item_type_id":"1","owner":"4","path":["409"],"pubdate":{"attribute_name":"公開日","attribute_value":"2001-07-01"},"publish_date":"2001-07-01","publish_status":"0","recid":"2414","relation_version_is_last":true,"title":["The nature of the Grenville-age charnockitic A-type magmatism from the Natal, Namaqua and Maud Belts of southern Africa and western Dronning Maud Land, Antarctica"],"weko_creator_id":"4","weko_shared_id":4},"updated":"2023-07-25T14:28:05.233169+00:00"}