{"created":"2023-07-27T06:58:36.600935+00:00","id":57346,"links":{},"metadata":{"_buckets":{"deposit":"60d32f8a-c053-40aa-bacd-578a7e73c7ed"},"_deposit":{"created_by":18,"id":"57346","owners":[18],"pid":{"revision_id":0,"type":"depid","value":"57346"},"status":"published"},"_oai":{"id":"oai:kanazawa-u.repo.nii.ac.jp:00057346","sets":["934:935:937"]},"author_link":["100569","1845","14173","100393","2310","17481","15592"],"item_4_biblio_info_8":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2018-11-15","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"11","bibliographicPageEnd":"946","bibliographicPageStart":"941","bibliographicVolumeNumber":"124","bibliographic_titles":[{"bibliographic_title":"地質学雑誌"},{"bibliographic_title":"The Journal of the Geological Society of Japan","bibliographic_titleLang":"en"}]}]},"item_4_creator_33":{"attribute_name":"著者別表示","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"Morishita, Tomoaki"}],"nameIdentifiers":[{},{}]},{"creatorNames":[{"creatorName":"町, 澄秋"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Guotana, Juan Miguel"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Tamura, Akihiro"}],"nameIdentifiers":[{},{}]}]},"item_4_description_21":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"Boulders of biotite-phenocryst-rich, high-K basaltic rock were discovered in the upper stream of the Kuzuryu River in Katsuyama City, Fukui Prefecture. The biotite phenocrysts are zoned, with pale brown cores and dark brown margins. Relics of mafic minerals, replaced by carbonate minerals, contain chromian spinel. Although the primary chemical composition is affected by the formation of secondary minerals such as carbonate, the SiO2 and K2O contents of the studied rock are 48-49 wt% and 3.6 wt%, respectively, which are within the chemical range of absarokite. Chondrite-normalized rare earth element and primitive-mantle-normalized trace element patterns of the studied volcanic rocks are characterized by high LREEs/HREEs, high concentrations of LILEs, and negative anomalies of HFSEs (Nb, Ti). These petrological and geochemical characteristics represent a primary composition that has never before been reported in the Hokuriku district.","subitem_description_type":"Abstract"}]},"item_4_description_5":{"attribute_name":"提供者所属","attribute_value_mlt":[{"subitem_description":"金沢大学理工研究域自然システム学系","subitem_description_type":"Other"}]},"item_4_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.24517/00063616","subitem_identifier_reg_type":"JaLC"}]},"item_4_publisher_17":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"日本地質学会 The Geological Society of Japan"}]},"item_4_relation_12":{"attribute_name":"DOI","attribute_value_mlt":[{"subitem_relation_type":"isIdenticalTo","subitem_relation_type_id":{"subitem_relation_type_id_text":"10.5575/geosoc.2018.0031","subitem_relation_type_select":"DOI"}}]},"item_4_relation_28":{"attribute_name":"関連URI","attribute_value_mlt":[{"subitem_relation_name":[{"subitem_relation_name_text":"http://www.geosociety.jp"}],"subitem_relation_type_id":{"subitem_relation_type_id_text":"http://www.geosociety.jp","subitem_relation_type_select":"URI"}},{"subitem_relation_name":[{"subitem_relation_name_text":"https://www.jstage.jst.go.jp/browse/geosoc/-char/ja/"}],"subitem_relation_type_id":{"subitem_relation_type_id_text":"https://www.jstage.jst.go.jp/browse/geosoc/-char/ja/","subitem_relation_type_select":"URI"}}]},"item_4_rights_23":{"attribute_name":"権利","attribute_value_mlt":[{"subitem_rights":"Copyright © 日本地質学会 The Geological Society of Japan"}]},"item_4_source_id_11":{"attribute_name":"NCID","attribute_value_mlt":[{"subitem_source_identifier":"AN00141768","subitem_source_identifier_type":"NCID"}]},"item_4_source_id_9":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"0016-7630","subitem_source_identifier_type":"ISSN"},{"subitem_source_identifier":" 1349-9963","subitem_source_identifier_type":"ISSN"}]},"item_4_version_type_25":{"attribute_name":"著者版フラグ","attribute_value_mlt":[{"subitem_version_resource":"http://purl.org/coar/version/c_970fb48d4fbd8a85","subitem_version_type":"VoR"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"森下, 知晃"}],"nameIdentifiers":[{},{}]},{"creatorNames":[{"creatorName":"町, 澄秋"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"ファン, ミゲル グオターナ"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"田村, 明弘"}],"nameIdentifiers":[{},{}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2021-08-30"}],"displaytype":"detail","filename":"SC-PR-MORISHITA-T-941.pdf","filesize":[{"value":"5.0 MB"}],"format":"application/pdf","licensetype":"license_11","mimetype":"application/pdf","url":{"label":"SC-PR-MORISHITA-T-941.pdf","url":"https://kanazawa-u.repo.nii.ac.jp/record/57346/files/SC-PR-MORISHITA-T-941.pdf"},"version_id":"d2933152-0f8f-4bf1-9fac-583ba7eee588"}]},"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":"journal article","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_title":"福井県勝山市九頭竜川上流地域の黒雲母斑晶に富む高カリウム玄武岩質転石","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"福井県勝山市九頭竜川上流地域の黒雲母斑晶に富む高カリウム玄武岩質転石"},{"subitem_title":"Biotite phenocryst-rich high-K basaltic boulder from upper stream of the Kuzuryu River in Katsuyama City, Fukui Prefecture","subitem_title_language":"en"}]},"item_type_id":"4","owner":"18","path":["937"],"pubdate":{"attribute_name":"公開日","attribute_value":"2021-08-30"},"publish_date":"2021-08-30","publish_status":"0","recid":"57346","relation_version_is_last":true,"title":["福井県勝山市九頭竜川上流地域の黒雲母斑晶に富む高カリウム玄武岩質転石"],"weko_creator_id":"18","weko_shared_id":-1},"updated":"2023-07-27T15:00:38.010847+00:00"}