{"created":"2021-03-01T06:06:57.060985+00:00","id":3203,"links":{},"metadata":{"_buckets":{"deposit":"6c567d6b-e47a-4862-b805-ddcdc11260f1"},"_deposit":{"id":"3203","owners":[],"pid":{"revision_id":0,"type":"depid","value":"3203"},"status":"published"},"_oai":{"id":"oai:niigata-u.repo.nii.ac.jp:00003203","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":"Cooling process of the basal tonalite magma, 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":"665","bibliographicPageStart":"654","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":"The low-pressure / high temperature type Hidaka Metamorphic Belt (HMB) in Hokkaido, northern Japan, re@resents a tilted crustal section of a magmatic arc of Tertiary age. Exposed crustal section forms deplex structure which was formed by the uplift tectonic process. Syntectonic tonalite magma intrudes along the floor thrust, ramp, and roof thrust of the crustal-scale duplex. The tonalite magma was generated by anatexis of the unexposed lowermost crust. Pyroxene-bearing tonalites (basal tonalite bodey) is distributed in the Niikappu river region, northern part of the Hidaka Metamorphic Belt. The various evidences that show a cooling process can be observed within the tonalite body, such as the orthopyroxene pseudomorth and the aplite veins. Cooling process of the tonalite body has been revealed from these texures. The P-T-t paths of the syn-tectonic tonalite suite and the metamorphic layer show the uplift teconics of the crust. A P-T-t path of the delaminated lowermost crust also can be presumed.","subitem_description_type":"Abstract"},{"subitem_description":"日高変成帯は，第三紀の火成弧の地殻断面であると見なされている，シンテクトニックなトーナル岩マグマは地殻規模のデュープレックス構造のフロアースラスト，ランプ，ルーフスラストに沿って迸入している．このトーナル岩マグマは露出していない最下部地殻のアナテクシスによって生じた. 日高変成帯北部の新冠川地域には，含輝石卜一ナル岩類（最下部トーナル岩体） が分布している．このトーナル岩体には，斜方輝石の仮像や，アプライト脈などの様々な冷却過程を示す証拠を見ることが出来る．これらの組織から，このトーナル岩体の冷却過程が明らかになった．シンテクトニックなトーナル岩体と，変成岩層のP −T−t 経路は地殻の上昇テクトニクスを示している，一方，デラミネーションを起こした最下部地殻のP −T −t 経路も推定することが可能である.","subitem_description_type":"Abstract"}]},"item_5_full_name_3":{"attribute_name":"著者別名","attribute_value_mlt":[{"nameIdentifiers":[{"nameIdentifier":"41424","nameIdentifierScheme":"WEKO"}],"names":[{"name":"Shimura, Toshiaki"}]},{"nameIdentifiers":[{"nameIdentifier":"41425","nameIdentifierScheme":"WEKO"}],"names":[{"name":"Osanai, Yasuhito"}]},{"nameIdentifiers":[{"nameIdentifier":"41426","nameIdentifierScheme":"WEKO"}],"names":[{"name":"Toyoshima, Tsuyoshi"}]},{"nameIdentifiers":[{"nameIdentifier":"41427","nameIdentifierScheme":"WEKO"}],"names":[{"name":"Owada, Masaaki"}]},{"nameIdentifiers":[{"nameIdentifier":"41428","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/110004863783","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":"志村, 俊昭"}],"nameIdentifiers":[{"nameIdentifier":"41419","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"小山内, 康人"}],"nameIdentifiers":[{"nameIdentifier":"41420","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"豊島, 剛志"}],"nameIdentifiers":[{"nameIdentifier":"41421","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"大和田, 正明"}],"nameIdentifiers":[{"nameIdentifier":"41422","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"小松, 正幸"}],"nameIdentifiers":[{"nameIdentifier":"41423","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":"110004863783.pdf","filesize":[{"value":"3.9 MB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"110004863783.pdf","url":"https://niigata-u.repo.nii.ac.jp/record/3203/files/110004863783.pdf"},"version_id":"f165893e-4c7c-4a63-84f4-fd090e8c0d11"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"cooling process","subitem_subject_scheme":"Other"},{"subitem_subject":"delamination","subitem_subject_scheme":"Other"},{"subitem_subject":"duplex","subitem_subject_scheme":"Other"},{"subitem_subject":"granulite","subitem_subject_scheme":"Other"},{"subitem_subject":"Hidaka metamorphic belt","subitem_subject_scheme":"Other"},{"subitem_subject":"P-T-t path","subitem_subject_scheme":"Other"},{"subitem_subject":"tonalite","subitem_subject_scheme":"Other"},{"subitem_subject":"tourmaline","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":"日高変成帯,最下部トーナル岩マグマの冷却プロセス(<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":"日高変成帯,最下部トーナル岩マグマの冷却プロセス(<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":"日高変成帯,最下部トーナル岩マグマの冷却プロセス(<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":"3203","relation_version_is_last":true,"title":["日高変成帯,最下部トーナル岩マグマの冷却プロセス(<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":"2022-12-15T03:36:21.498303+00:00"}