{"@context":{"@vocab":"https://cir.nii.ac.jp/schema/1.0/","rdfs":"http://www.w3.org/2000/01/rdf-schema#","dc":"http://purl.org/dc/elements/1.1/","dcterms":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","prism":"http://prismstandard.org/namespaces/basic/2.0/","cinii":"http://ci.nii.ac.jp/ns/1.0/","datacite":"https://schema.datacite.org/meta/kernel-4/","ndl":"http://ndl.go.jp/dcndl/terms/","jpcoar":"https://github.com/JPCOAR/schema/blob/master/2.0/"},"@id":"https://cir.nii.ac.jp/crid/1361699995284904832.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/0040-1951(81)90103-7"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:0040195181901037?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:0040195181901037?httpAccept=text/plain"}},{"identifier":{"@type":"NAID","@value":"80000935450"}}],"dc:title":[{"@value":"Subdivision of the hida metamorphic complex, central Japan, and its bearing on the geology of the Far East in pre-Sea of Japan time"}],"description":[{"notation":[{"@value":"Abstract   Petrological and structural characteristics of the regional metamorphic rocks in south-west Japan and in the Korean Peninsula make it possible to speculate on the geological correlation between Japan and the Asian continent prior to the opening of the Sea of Japan, a typical marginal sea. The Hida metamorphic complex, situated on the Sea of Japan side of southwest Japan, is subdivided into two distinct geological units, the Hida gneisses and the Unazuki schists. The Hida gneisses are polymetamorphosed Precambrian rocks, while the Unazuki schists occurring on its eastern and southern sides are low- to medium-grade metamorphic rocks originating from Upper Paleozoic deposits. Sedimentary facies and other geological features suggest that the Hida gneisses were the basemen of the Unazuki schists. Consequently, the geotectonic framework of southwest Japan is revised from north to south as follows: Hida gneiss region (Precambrian massif) Unazuki zone (late Permian intermed.    P  T    metamorphic belt) Circum-Hida tectonic zone (Mid- to Late Paleozoic melange zone) Mino-Tanba terrain (Late Paleozoic to Mesozoic geosynclinal region) and so on.  The Unazuki zone is similar to the Okcheon zone in the Korean Peninsula in respect of age, lithology and biofacies of sedimentary rocks as well as the age and type of regional metamorphism. Furthermore, the Hida gneisses and the Gyeonggi polymetamorphosed Precambrian gneisses in the Korean Peninsula are similar in the apparent baric type of metamorphism, radiometric ages and the relationship with the overlying metamorphosed formations. The similarity of the geotectonic frameworks of southwest Japan and the Korean Peninsula suggests that the Unazuki zone and the Okcheon zone once formed a continuous geotectonic unit. Thus we have a new geological coordinate in reconstructing the paleogeography prior to the opening of the Sea of Japan."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381699995284904832","@type":"Researcher","foaf:name":[{"@value":"Yoshikuni Hiroi"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00401951"}],"prism:publicationName":[{"@value":"Tectonophysics"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"1981-07","prism:volume":"76","prism:number":"3-4","prism:startingPage":"317","prism:endingPage":"333"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/","https://www.elsevier.com/legal/tdmrep-license"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:0040195181901037?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:0040195181901037?httpAccept=text/plain"}],"createdAt":"2003-08-07","modifiedAt":"2025-09-08","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360013168868040704","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Nature and timing of anatectic event of the Hida Belt (Japan): Constraints from titanite geochemistry and U-Pb age of clinopyroxene-bearing leucogranite"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707500184192","@type":"Article","resourceType":"学術雑誌論文(journal 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Craton"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565165811145856","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Timing and duration of regional metamorphism in the Kagasawa and Unazuki areas, Hida metamorphic complex, southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567185481761920","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"U–Pb zircon geochronology of the Hida gneiss and granites in the Kamioka area, Hida Belt"}]},{"@id":"https://cir.nii.ac.jp/crid/1360853567602488576","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The <scp>δ<sup>13</sup>C</scp>–<scp>δ<sup>18</sup>O</scp> variations in marble in the Hida Belt, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418519114073344","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@value":"Mantle diapir‐induced arc volcanism: The Ueno Basalts, Nomugi‐Toge and Hida volcanic suites, central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670319823646464","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@value":"Tectono‐metamorphic evolution of the Okcheon Metamorphic Belt, South Korea: Tectonic implications in East Asia"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204230440064","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Juvenile Japan: Hydrothermal Activity of the Hida-Gaien Belt Indicating Initiation of Subduction of Proto-Pacific Plate in ca. 520 Ma"},{"@language":"ja","@value":"日本列島の誕生場―古太平洋の沈み込み開始を示す飛騨外縁帯の５２０Ｍａの熱水活動―"},{"@language":"ja-Kana","@value":"ニホン レットウ ノ タンジョウバ コ タイヘイヨウ ノ シズミ コミ カイシ オ シメス ヒダ ガイエンタイ ノ 520Ma ノ ネッスイ カツドウ"},{"@value":"Hydrothermal activity of the Hida-Gaien belt indicating initiation of subduction of Proto-Pacific plate in ca. 520Ma"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204237127168","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Geotectonic Evolution of the Hida Marginal Belt, Central Japan: Reconstruction of the Oldest Pacific-type Orogeny of Japan"},{"@language":"ja","@value":"飛騨外縁帯の地質構造発達史―日本列島地質体最古の太平洋型造山運動の復元―"},{"@language":"ja-Kana","@value":"ヒダ ガイエンタイ ノ チシツ コウゾウ ハッタツシ : ニホン レットウ チシツタイ サイコ ノ タイヘイヨウガタ ゾウザン ウンドウ ノ フクゲン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204237574144","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Classification of Orogenic Belts: Constraints on the Reconstruction of Paleo-geotectonic Environments"},{"@language":"ja","@value":"造山帯の分類とその意義：古造構場復元の束縛条件"},{"@value":"造山帯の分類とその意義 : 古造構場復元の束縛条件 : 「丸山ほか : 太平洋型造山帯 : 新しい概念の提唱と地球史における時空分布」論文(地学雑誌,120巻,115-223)の追記"},{"@language":"ja-Kana","@value":"ゾウザンタイ ノ ブンルイ ト ソノ イギ : コゾウコウジョウ フクゲン ノ ソクバク ジョウケン : 「 マルヤマ ホカ : タイヘイヨウガタ ゾウザンタイ : アタラシイ ガイネン ノ テイショウ ト チキュウシ ニ オケル ジクウ ブンプ 」 ロンブン(チガク ザッシ,120カン,115-223)ノ ツイキ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204550439680","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"U-Pb dating of detrital zircons from the Sangun metamorphic rocks, Kyushu, Southwest Japan: An evidence for 1.9-2.0 Ga granite emplacement in the provenance."},{"@language":"ja-Kana","@value":"U-Pb dating of detrital zircons from th"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206234452096","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Pre-Neogene tectonics of the Japanese Islands from the viewpoint of palaeobiogeography."},{"@value":"古生物地理からみた日本列島の先新第三紀テクトニクス"},{"@language":"ja-Kana","@value":"コセイブツ チリ カラ ミタ ニホン レットウ ノ センシンダイ3キ テクトニ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206234563584","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Sedimentary facies and clast compositions of the Motodo Formation in the Hida-gaien Tectonic Zone, Fukui Prefecture, central Japan."},{"@value":"飛騨外縁帯，本戸累層の堆積相とれき種構成"},{"@language":"ja-Kana","@value":"ヒダ ガイエンタイ モトドルイソウ ノ タイセキソウ ト レキシュ コウセイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206234646016","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Staurolite-bearing sillimanite schist cobble from the Upper Jurassic Tetori Group in the Kuzuryu area, Hida Mountains, central Japan."},{"@language":"ja","@value":"飛騨山地九頭竜地域,上部ジュラ系手取層群中の十字石-珪線石片岩礫"},{"@language":"ja-Kana","@value":"Staurolite bearing sillimanite schist c"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206238024704","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Palaeozoic and Mesozoic tectonics of the Hida Gaien Belt, central Japan: Overview"},{"@language":"ja","@value":"飛騨外縁帯の古生代～中生代テクトニクスに関する従来の研究と今後の課題"},{"@language":"ja-Kana","@value":"ヒダ ガイエンタイ ノ コセイダイ チュウセイダイ テクトニクス ニ カンスル ジュウライ ノ ケンキュウ ト コンゴ ノ カダイ"},{"@value":"Paleozoic and Mesozoic tectonics of the Hida Gaien Belt, central Japan: Overview"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206238031616","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Outline of the shear zones in the Kuzuryu area, Hida Gaien belt, Fukui Prefecture, central Japan"},{"@language":"ja","@value":"飛騨外縁帯九頭竜地域の剪断帯群概報"},{"@language":"ja-Kana","@value":"ヒダ ガイエンタイ クズリュウ チイキ ノ 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Shiroumadake area, Hida Gaien belt, central Japan"},{"@language":"ja","@value":"飛騨外縁帯白馬岳地域のペルム系白馬岳層の層序および蛇紋岩との関係"},{"@language":"ja-Kana","@value":"ヒダ ガイエンタイ シロウマダケ チイキ ノ ペルムケイ シロウマダケソウ ノ ソウ ジョ オヨビ ジャモンガン ト ノ カンケイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206238342144","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Fossil-bearing limestone and garnet-bearing clastic rocks found at Nishiamada in Fukui City, central Japan and their significance"},{"@language":"ja","@value":"福井市西天田において見つかった含化石石灰岩および含ザクロ石砕屑岩とその意義"},{"@language":"ja-Kana","@value":"フクイシ ニシアマダ ニ オイテ ミツカッタ ガン カセキ セッカイガン オヨビ ガン ザクロイシ サイセツガン ト ソノ イギ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679206275072","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"History of Supercontinents and Its Relation to the Origin of japanese Islands"},{"@language":"ja","@value":"超大陸と日本列島の起源"},{"@language":"ja-Kana","@value":"チョウタイリク ト ニホン レットウ ノ キゲン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679207149184","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Paleozoic Subduction-related Metamorphism in Japan: New Insights and Perspectives"},{"@language":"ja","@value":"日本列島に記録された古生代高圧変成作用―新知見とこれから解決すべき問題点―"},{"@language":"ja-Kana","@value":"ニホン レットウ ニ キロク サレタ コセイダイ コウアツ ヘンセイ サヨウ シン チケン ト コレカラ カイケツ スベキ モンダイテン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681210681344","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Kinematic pictures of the ductile shear zones in the Hida terrane and their tectonic implication."},{"@value":"飛騨地帯の延性せん断帯の運動像とテクトニクス"},{"@language":"ja-Kana","@value":"ヒダ チタイ ノ エンセイ センダンタイ ノ ウンドウゾウ ト 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