{"created":"2021-03-01T06:06:56.937489+00:00","id":3201,"links":{},"metadata":{"_buckets":{"deposit":"c8452abd-d387-467b-bd39-4d798ce29604"},"_deposit":{"id":"3201","owners":[],"pid":{"revision_id":0,"type":"depid","value":"3201"},"status":"published"},"_oai":{"id":"oai:niigata-u.repo.nii.ac.jp:00003201","sets":["176:488:489","453:454"]},"item_5_alternative_title_1":{"attribute_name":"その他のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"Partial melting of high-grade metamorphic rocks in lower crustal part of the Hidaka Arc (Main Zone of the Hidaka metamorphic belt), northern Japan(<SPECIAL ISSUE>Recent Advances in Research of the Hidaka Collision Zone, Hokkaido, Northern Japan: Deep-Seated Processes and Tectonic Uplift (Part 1))"}]},"item_5_biblio_info_6":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2006-11","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"11","bibliographicPageEnd":"638","bibliographicPageStart":"623","bibliographicVolumeNumber":"112","bibliographic_titles":[{"bibliographic_title":"地質学雑誌"},{"bibliographic_title":"地質学雑誌","bibliographic_titleLang":"en"}]}]},"item_5_description_4":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"Lower crustal part of the Hidaka Arc (Hidaka metamorphic belt) is composed of the granulite-facies unit (zone IV) and the main anatexis zone. The former can be observed on the surface, while the latter is considered to be existed beneath the Hidaka Main Thrust by the evidence of restitic Gr-Opx granulites as xenoliths included in intrusive anatectic tonalities. In pelitic granulites of zone IV, Bt-dehydration melting took place with forming leucosomes including euhedral Opx, An-rich PI and Crd. Intercalated mafic granulites in zone IV also show the Hbl-dehydration melting and Opx-bearing leucosome formation. A small scale partial melting in zone IV is identified, where the produced melt would be effected to make plastic condition of lower crustal rocks and to form duplex structure in the lower crust of the Hidaka Arc. Partial molten melts derived from the main anatexis zone moved and assembled to form tonalitic magmas with peraluminous S-type and metaluminous I-type signatures, which intruded into the shallower crustal level along the floor-thrust and roof-thrust of duplex structure.","subitem_description_type":"Abstract"},{"subitem_description":"日高変成帯主帯下部地殻は,現在地表に露出しているグラニュライト相変成岩分布域(IV帯)および主要部分溶融帯からなる.後者は現在地表に露出しないが,レスタイトと見なされるザクロ石-斜方輝石グラニュライト(トーナル岩の包有物)などから,その存在が推定される.IV帯の泥質グラニュライトでは,黒雲母の脱水溶融反応が起こり,自形の斜方輝石やAn成分に富む斜長石および菫青石を含む様々なリューコゾームが形成された.互層する苦鉄質グラニュライトでもホルンブレンドの脱水溶融が起こり,生成したメルトはブーダンネックなどへ濃集し,含斜方輝石リューコゾームを形成したと見なされる.IV帯における部分溶融度は比較的小さいが,生成したメルトは地殻下部岩石の塑性流動化とデュープレックス構造の形成に関与した.主要部分溶融帯で生成したメルトは移動・濃集してトーナル岩マグマとして挙動し,シート状岩体を形成した.","subitem_description_type":"Abstract"}]},"item_5_full_name_3":{"attribute_name":"著者別名","attribute_value_mlt":[{"nameIdentifiers":[{"nameIdentifier":"41403","nameIdentifierScheme":"WEKO"}],"names":[{"name":"Osanai, Yasuhito"}]},{"nameIdentifiers":[{"nameIdentifier":"41404","nameIdentifierScheme":"WEKO"}],"names":[{"name":"Owada, Masaaki"}]},{"nameIdentifiers":[{"nameIdentifier":"41405","nameIdentifierScheme":"WEKO"}],"names":[{"name":"Shimura, Toshiaki"}]},{"nameIdentifiers":[{"nameIdentifier":"41406","nameIdentifierScheme":"WEKO"}],"names":[{"name":"Nakano, Nobuhiko"}]},{"nameIdentifiers":[{"nameIdentifier":"41407","nameIdentifierScheme":"WEKO"}],"names":[{"name":"Kawanami, Seishi"}]},{"nameIdentifiers":[{"nameIdentifier":"41408","nameIdentifierScheme":"WEKO"}],"names":[{"name":"Komatsu, Masayuki"}]}]},"item_5_publisher_7":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"日本地質学会"}]},"item_5_relation_31":{"attribute_name":"異版である","attribute_value_mlt":[{"subitem_relation_type":"isVersionOf","subitem_relation_type_id":{"subitem_relation_type_id_text":"http://ci.nii.ac.jp/naid/110004863781","subitem_relation_type_select":"URI"}}]},"item_5_rights_15":{"attribute_name":"権利","attribute_value_mlt":[{"subitem_rights":"Copyright(C)2006 日本地質学会"},{"subitem_rights":"本文データは学協会の許諾に基づきCiNiiから複製したものである"}]},"item_5_select_19":{"attribute_name":"著者版フラグ","attribute_value_mlt":[{"subitem_select_item":"publisher"}]},"item_5_source_id_11":{"attribute_name":"書誌レコードID","attribute_value_mlt":[{"subitem_source_identifier":"AN00141768","subitem_source_identifier_type":"NCID"}]},"item_5_source_id_9":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"00167630","subitem_source_identifier_type":"ISSN"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"小山内, 康人"}],"nameIdentifiers":[{"nameIdentifier":"41397","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"大和田, 正明"}],"nameIdentifiers":[{"nameIdentifier":"41398","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"志村, 俊昭"}],"nameIdentifiers":[{"nameIdentifier":"41399","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"中野, 伸彦"}],"nameIdentifiers":[{"nameIdentifier":"41400","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"川浪, 聖志"}],"nameIdentifiers":[{"nameIdentifier":"41401","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"小松, 正幸"}],"nameIdentifiers":[{"nameIdentifier":"41402","nameIdentifierScheme":"WEKO"}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2019-07-30"}],"displaytype":"detail","filename":"110004863781.pdf","filesize":[{"value":"5.8 MB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"110004863781.pdf","url":"https://niigata-u.repo.nii.ac.jp/record/3201/files/110004863781.pdf"},"version_id":"51d573bb-8732-4cad-bfab-665da71422ac"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"granulite-facies","subitem_subject_scheme":"Other"},{"subitem_subject":"partial melting","subitem_subject_scheme":"Other"},{"subitem_subject":"Opx-bearing leucosome","subitem_subject_scheme":"Other"},{"subitem_subject":"tonalite magma","subitem_subject_scheme":"Other"},{"subitem_subject":"lower crust","subitem_subject_scheme":"Other"},{"subitem_subject":"Hidaka metamorphic belt","subitem_subject_scheme":"Other"}]},"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":"日高島弧(日高変成帯主帯)下部地殻における高度変成岩の部分溶融(<特集>日高衝突帯研究の最近の進歩(1)-その深部過程と上昇過程)","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"日高島弧(日高変成帯主帯)下部地殻における高度変成岩の部分溶融(<特集>日高衝突帯研究の最近の進歩(1)-その深部過程と上昇過程)"},{"subitem_title":"日高島弧(日高変成帯主帯)下部地殻における高度変成岩の部分溶融(<特集>日高衝突帯研究の最近の進歩(1)-その深部過程と上昇過程)","subitem_title_language":"en"}]},"item_type_id":"5","owner":"1","path":["454","489"],"pubdate":{"attribute_name":"公開日","attribute_value":"2014-09-09"},"publish_date":"2014-09-09","publish_status":"0","recid":"3201","relation_version_is_last":true,"title":["日高島弧(日高変成帯主帯)下部地殻における高度変成岩の部分溶融(<特集>日高衝突帯研究の最近の進歩(1)-その深部過程と上昇過程)"],"weko_creator_id":"1","weko_shared_id":null},"updated":"2022-12-15T03:36:21.921584+00:00"}