{"created":"2023-06-19T09:37:18.891192+00:00","id":883,"links":{},"metadata":{"_buckets":{"deposit":"ca3a359a-e27a-453f-8ccb-9d66d285360e"},"_deposit":{"created_by":2,"id":"883","owners":[2],"pid":{"revision_id":0,"type":"depid","value":"883"},"status":"published"},"_oai":{"id":"oai:ngu.repo.nii.ac.jp:00000883","sets":["1:12:204"]},"author_link":["961","2259","2258"],"item_10002_alternative_title_1":{"attribute_name":"その他（別言語等）のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"ボヘミアサンカイナンブLhenice shear zoneニサンスルデイシツヘンマガンノゼンガンカガクソセイ"}]},"item_10002_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2017-01-31","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"2","bibliographicPageEnd":"68","bibliographicPageStart":"51","bibliographicVolumeNumber":"53","bibliographic_titles":[{"bibliographic_title":"名古屋学院大学論集　人文・自然科学篇"},{"bibliographic_title":"THE NAGOYA GAKUIN DAIGAKU RONSHU; Journal of Nagoya Gakuin University; HUMANITIES and NATURAL SCIENCES","bibliographic_titleLang":"en"}]}]},"item_10002_description_5":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"　 Whole rock chemical analysis was carried out for sillimanite-cordierite-biotite-garnet (Sil-Crd-Bt-Grt) gneisses at Ktiš in the Lhenice shear zone of the southern Bohemian Massif, Czech Republic, in order to consider the origin of this rock.  The Sil-Crd-Bt-Grt gneiss shows a variety of lithotype mainly controlled by modal amount and grain size of main constituent minerals, resulting in the wide chemical variation of SiO2 content even in one outcrop from mafic composition (48.5 wt％) of a melanocratic layer with coarse-grained Grt to felsic composition (76.9 wt％) of a leucocratic vein.  Petrology of the Sil-Crd-Bt-Grt gneiss and common occurrence of the leucosome in the outcrop suggest that the study rock suffered the partial melting during the exhumation stage.  Available geochemical data suggest that leucocratic lithotypes with SiO2 contents from 70.3 to 76.9 wt％ were formed by the partial melting of the protolith and melanocratic types with SiO2 contents from 48.5 to 60.6 wt％, which include the main lithotype, were the residue.  Therefore, leucocratic/melanocratic layer intercalations with SiO2 contents from 57.0 to 65.0 wt％ would most likely represent the chemical composition of the protolith of Ktiš gneiss.  Several lines of chemical features of the leucocratic/melanocratic layer intercalation suggest that the protolith would be a mixture of greywacke and pelite with moderate aluminum saturation index (ASI) value and is characterized by extreme high Fe2O3 compared with continental and trench fill sediments.","subitem_description_type":"Abstract"}]},"item_10002_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.15012/00000872","subitem_identifier_reg_type":"JaLC"}]},"item_10002_publisher_8":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"名古屋学院大学総合研究所"}]},"item_10002_source_id_9":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"0385-0056","subitem_source_identifier_type":"ISSN"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"小林, 記之"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"平島, 崇男"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"マルチン, スフォイッカ"}],"nameIdentifiers":[{}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2017-02-09"}],"displaytype":"detail","filename":"jinbun_vol5302_04.pdf","filesize":[{"value":"687.6 kB"}],"format":"application/pdf","license_note":"Copyright (c) 2017 小林記之, 平島崇男,マルチン・スフォイッカ","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"jinbun_vol5302_04.pdf","url":"https://ngu.repo.nii.ac.jp/record/883/files/jinbun_vol5302_04.pdf"},"version_id":"4011c2a9-a5c8-4085-92dc-427041dfd405"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"whole rock","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"Bohemian Massif","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"Lhenice shear zone","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"Protolith","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":"ボヘミア山塊南部Lhenice shear zoneに産する泥質片麻岩の全岩化学組成","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"ボヘミア山塊南部Lhenice shear zoneに産する泥質片麻岩の全岩化学組成"},{"subitem_title":"Geochemical Features of Pelitic Gneiss in the Lhenice Shear Zone (Moldanubian Zone of the Southern Bohemian Massif)","subitem_title_language":"en"}]},"item_type_id":"10002","owner":"2","path":["204"],"pubdate":{"attribute_name":"公開日","attribute_value":"2017-02-09"},"publish_date":"2017-02-09","publish_status":"0","recid":"883","relation_version_is_last":true,"title":["ボヘミア山塊南部Lhenice shear zoneに産する泥質片麻岩の全岩化学組成"],"weko_creator_id":"2","weko_shared_id":2},"updated":"2023-06-19T09:47:20.011646+00:00"}