{"@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/1390013430232867840.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.2465/jmps.220630"}},{"identifier":{"@type":"URI","@value":"https://www.jstage.jst.go.jp/article/jmps/118/1/118_220630/_pdf"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@language":"en","@value":"U-Pb zircon ages of metamorphic rocks and granitoids from the Nagato Tectonic Zone in Yamaguchi, southwest Japan: Implication for the geological correlation with the Kurosegawa Tectonic Belt"}],"dc:language":"en","description":[{"type":"abstract","notation":[{"@language":"en","@value":"<p>The metamorphic and plutonic rocks within a serpentinite mélange in the Nagato Tectonic Zone, Yamaguchi prefecture, southwest Japan have been known as a part of the early Paleozoic rock record in Japan. Thus, they play an important role in deciphering the tectonic evolution of proto-Japan. This study determined their U-Pb zircon ages to deduce the origin and geological significance of the Nagato Tectonic Zone. The results of the petrographic observation and LA-ICP-MS U-Pb zircon dating revealed the occurrences of the massive amphibolite originated from the 460 Ma mafic igneous rock, two-mica tonalites formed at 470-460 Ma in association with some xenocrystic zircon grains, and low-grade metasedimentary rocks including detrital zircon grains of 2460-400 Ma. The lithology, petrographic characteristics, and U-Pb zircon ages of these constituent rocks in the Nagato Tectonic Zone are well comparable with the blocks within serpentinite mélange in the Kurosegawa Tectonic Belt, rather than the Hida Gaien Belt which has been considered to form a single geological unit with the Nagato Tectonic Zone as the Sangun-Renge metamorphic belt or Nagato-Renge belt. It implies the Nagato Tectonic Zone could be regarded as an isolated fragment of the Kurosegawa Tectonic Belt. The features of detrital age spectra and Ordovician magmatism in the Nagato Tectonic Zone and Kurosegawa Tectonic Belt provide the possibility of the development of their granitoids and protoliths of metamorphic rocks at the active continental margin of the South China craton.</p>"}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1410013430232867841","@type":"Researcher","foaf:name":[{"@language":"en","@value":"KITANO Ippei"}],"jpcoar:affiliationName":[{"@language":"en","@value":"The Hokkaido University Museum, Hokkaido University"},{"@language":"en","@value":"Division of Earth Sciences, Faculty of Social and Cultural Studies, Kyushu University"}]},{"@id":"https://cir.nii.ac.jp/crid/1030003658402043394","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"80183771"},{"@type":"NRID","@value":"1000080183771"},{"@type":"ORCID","@value":"0000-0001-8044-2543"},{"@type":"NRID","@value":"9000002194294"},{"@type":"NRID","@value":"9000402492000"},{"@type":"NRID","@value":"9000022836885"},{"@type":"NRID","@value":"9000022836796"},{"@type":"NRID","@value":"9000283726174"},{"@type":"NRID","@value":"9000329013446"},{"@type":"NRID","@value":"9000022835745"},{"@type":"NRID","@value":"9000347138348"},{"@type":"NRID","@value":"9000397721149"},{"@type":"NRID","@value":"9000015504937"},{"@type":"NRID","@value":"9000240048214"},{"@type":"NRID","@value":"9000339175182"},{"@type":"NRID","@value":"9000329013444"},{"@type":"NRID","@value":"9000002257214"},{"@type":"NRID","@value":"9000347082823"},{"@type":"NRID","@value":"9000258744274"},{"@type":"NRID","@value":"9000248249004"},{"@type":"NRID","@value":"9000022836695"},{"@type":"NRID","@value":"9000335196232"},{"@type":"NRID","@value":"9000022838539"},{"@type":"NRID","@value":"9000021304777"},{"@type":"NRID","@value":"9000259311776"},{"@type":"NRID","@value":"9000020136169"},{"@type":"NRID","@value":"9000329013464"},{"@type":"NRID","@value":"9000283099829"},{"@type":"NRID","@value":"9000006567035"},{"@type":"NRID","@value":"9000022835699"},{"@type":"NRID","@value":"9000412114969"},{"@type":"NRID","@value":"9000262359466"},{"@type":"NRID","@value":"9000335196140"},{"@type":"NRID","@value":"9000329013428"},{"@type":"NRID","@value":"9000261037102"},{"@type":"NRID","@value":"9000347138135"},{"@type":"NRID","@value":"9000402492016"},{"@type":"NRID","@value":"9000002142759"},{"@type":"NRID","@value":"9000022254691"},{"@type":"NRID","@value":"9000323295395"},{"@type":"NRID","@value":"9000329013458"},{"@type":"NRID","@value":"9000259311782"},{"@type":"NRID","@value":"9000020236530"},{"@type":"NRID","@value":"9000001319460"},{"@type":"NRID","@value":"9000022838719"},{"@type":"NRID","@value":"9000329013454"},{"@type":"NRID","@value":"9000396138775"},{"@type":"NRID","@value":"9000405665129"},{"@type":"NRID","@value":"9000254151442"},{"@type":"NRID","@value":"9000240048307"},{"@type":"NRID","@value":"9000365024373"},{"@type":"NRID","@value":"9000365023890"},{"@type":"NRID","@value":"9000365023892"},{"@type":"NRID","@value":"9000365024387"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/Osanai0371"}],"foaf:name":[{"@language":"en","@value":"OSANAI Yasuhito"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Division of Earth Sciences, Faculty of Social and Cultural Studies, Kyushu University"}]},{"@id":"https://cir.nii.ac.jp/crid/1410013430232867843","@type":"Researcher","foaf:name":[{"@language":"en","@value":"NAKANO Nobuhiko"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Division of Earth Sciences, Faculty of Social and Cultural Studies, Kyushu University"}]},{"@id":"https://cir.nii.ac.jp/crid/1410013430232867842","@type":"Researcher","foaf:name":[{"@language":"en","@value":"KATO Ryosuke"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Graduate School of Integrated Sciences for Global Society, Kyushu University"},{"@language":"en","@value":"Kanto Branch, Dia Consultants Co. Ltd."}]},{"@id":"https://cir.nii.ac.jp/crid/1410013430232867844","@type":"Researcher","foaf:name":[{"@language":"en","@value":"BUI THI SINH Vuong"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Graduate School of Integrated Sciences for Global Society, Kyushu University"},{"@language":"en","@value":"Institute of Geological Sciences, Vietnam Academy of Science and Technology"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"13456296"},{"@type":"LISSN","@value":"13456296"},{"@type":"EISSN","@value":"13493825"}],"prism:publicationName":[{"@language":"en","@value":"Journal of Mineralogical and Petrological Sciences"},{"@language":"en","@value":"Journal of Mineralogical and Petrological Sciences"}],"dc:publisher":[{"@language":"en","@value":"Japan Association of Mineralogical Sciences"},{"@language":"ja","@value":"一般社団法人　日本鉱物科学会"}],"prism:publicationDate":"2023","prism:volume":"118","prism:number":"1","prism:startingPage":"n/a"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","url":[{"@id":"https://www.jstage.jst.go.jp/article/jmps/118/1/118_220630/_pdf"}],"availableAt":"2023","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=U-Pb%20zircon%20ages","dc:title":"U-Pb zircon ages"},{"@id":"https://cir.nii.ac.jp/all?q=Metamorphic%20rocks","dc:title":"Metamorphic rocks"},{"@id":"https://cir.nii.ac.jp/all?q=Granitoids","dc:title":"Granitoids"},{"@id":"https://cir.nii.ac.jp/all?q=Nagato%20Tectonic%20Zone","dc:title":"Nagato Tectonic Zone"},{"@id":"https://cir.nii.ac.jp/all?q=Kurosegawa%20Tectonic%20Belt","dc:title":"Kurosegawa Tectonic Belt"}],"project":[{"@id":"https://cir.nii.ac.jp/crid/1040000781896629120","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"16H02743"},{"@type":"JGN","@value":"JP16H02743"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-16H02743/"}],"notation":[{"@language":"ja","@value":"微小領域マルチアイソトープ年代測定による北部アジア地域の大陸衝突過程の精密解析"},{"@language":"en","@value":"Precise multi isotope geochronological analyses of continental collision process in northern Asia"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360011144494909568","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Composition of Zircon and Igneous and Metamorphic Petrogenesis"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011146176574720","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Prograde and Retrograde P-T Paths of the Late Paleozoic Glaucophane Eclogite from the Renge Metamorphic Belt, Hida Mountains, Southwestern 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Timely"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262943310248832","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Precise U‐Pb ages of Duluth Complex and related mafic intrusions, northeastern Minnesota: Geochronological insights to physical, petrogenetic, paleomagnetic, and tectonomagmatic processes associated with the 1.1 Ga Midcontinent Rift System"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825895303783168","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Abbreviations for names of rock-forming minerals"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107370235131136","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"TEMORA 1: a new zircon standard for Phanerozoic U–Pb geochronology"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206216327040","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"K-A dating on the granitic rock from Mine City, Yamaguchi Prefecture"},{"@value":"山口県美禰市産花崗岩質岩のK-A年代"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206237775744","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Die Kurosegawa-Zone:(Untersuchugen uber das Chichibu-Terrain in shikoku-III)"},{"@value":"黒瀬川構造帯:(四国秩父累帯の研究III)"},{"@language":"ja-Kana","@value":"シコク チチブルイタイ ノ ケンキュウ 3"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206238114560","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"秋吉地域の山口層群,大田層"},{"@language":"en","@value":"Ota Formation of the Yamaguchi Group in the Akiyoshi District"},{"@language":"ja-Kana","@value":"アキヨシ チイキ ノ ヤマグチソウグン , オオタソウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679207522048","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Geotectonic Subdivision of the Japanese Islands Revisited: Categorization and Definition of Elements and Boundaries of Pacific-type (Miyashiro-type) Orogen"},{"@language":"ja","@value":"日本列島の地体構造区分再訪―太平洋型（都城型）造山帯構成単元および境界の分類・定義―"},{"@language":"ja-Kana","@value":"ニホン レットウ ノ ジタイ コウゾウ クブン サイホウ タイヘイヨウガタ ミヤシロガタ ゾウザンタイ コウセイ タンゲン オヨビ キョウカイ ノ ブンルイ テイギ"},{"@value":"Geotectonic subdivision of the Japanese Islands revisited: Categorization and definition of elements and boundaries of Pacific-type (Miyashiro-type) orogeny"},{"@value":"Geotectonic subdivision of the Japanese Islands revisited and relevant new perspective: categorization and definition of elements and boundaries of a Pacific-type (Miyashiro-type) orogen"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681191902336","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"K-Ar ages of Sangun metamorphic rocks in Yamaguchi Prefecture and their geologic significance."},{"@language":"ja","@value":"山口県における三郡変成岩のK-Ar年代とその地質学的意義"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681192779264","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Rb-Sr dating on the rocks in Japan (I),"},{"@value":"Rb-Srによる地質年令(I)"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681211575936","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Find of boundary thrust between 300Ma high-P/T type schists and weakly metamorphosed Permian accretionary complex in the Nagato tectonic zone, Southwest Japan."},{"@value":"長門構造帯，３００Ｍａ低温高圧型片岩類と弱変成ペルム紀付加体間の境界スラストの発見"},{"@language":"ja-Kana","@value":"ナガト コウゾウタイ 300Ma テイオン コウアツガタ ヘンガンルイ ト ジ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681214783744","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Early Permian radiolarians from mudstone at Hisage in the Dai area, Nagato Tectonic Zone, Southwest Japan"},{"@language":"ja","@value":"長門構造帯台地域久下の泥岩から産出した前期ペルム紀放散虫化石"},{"@language":"ja-Kana","@value":"ナガト コウゾウタイ ダイチイキ ヒサゲ ノ デイガン カラ サンシュツ シタ ゼンキ ペルムキ ホウサンチュウ カセキ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681214824192","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"長門構造帯より紡錘虫化石の発見"},{"@language":"en","@value":"Finding of Fusulinids from Nagato Tectonic Zone"},{"@language":"ja-Kana","@value":"ナガト コウゾウタイ ヨリ ボウスイチュウ カセキ ノ ハッケン タンポウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681215518976","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Naguri Fault Zone as the Kurosegawa Terrane in the eastern part of the Kanto Mountains, central Japan"},{"@value":"関東山地東縁部の黒瀬川地帯-名栗断層帯"},{"@language":"ja-Kana","@value":"カントウ サンチ トウエンブ ノ クロセガワ チタイ ナグリ ダンソウタイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681217961472","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"LA-ICP-MS U–Pb zircon and FE-EPMA U–Th–Pb monazite dating of pelitic granulites from the Mt. Ukidake area, Sefuri Mountains, northern Kyushu"},{"@language":"ja","@value":"浮嶽地域に産する泥質グラニュライトのLA-ICP-MS U－Pbジルコン年代とFE-EPMA U－Th－Pbモナザイト年代"},{"@value":"LA-ICP-MS U–Pb zircon and FE-EPMA U–Th–Pb monazite dating on pelitic granulites from the Mt. Ukidake area, Sefuri Mountains, northern Kyushu"},{"@value":"LA-ICP-MS U-Pb zircon and FE-EPMA U-Th-Pb monazite datings on pelitic granulites from the Mt. Ukidake area, Sefuri Mountains, northern Kyushu"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681503036800","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"LA-ICP-MS zircon U-Pb geochronology of Paleozoic granitic rocks and related igneous rocks from the Kurosegawa tectonic belt in Kyushu, Southwest Japan"},{"@language":"ja","@value":"九州・黒瀬川構造帯における古生代花崗岩類および関連火成岩類の LA-ICP-MS ジルコン U-Pb 年代"},{"@language":"ja-Kana","@value":"キュウシュウ ・ クロセガワ コウゾウタイ ニ オケル コセイダイ ハナオカガンルイ オヨビ カンレン カセイガンルイ ノ LA-ICP-MS ジルコン U-Pb ネンダイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681523215232","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"U-Pb detrital zircon dating of pelitic schists and quartzite from the Kurosegawa Tectonic Zone, Southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681523785856","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"In–situ U–Pb zircon age dating deciphering the formation event of the omphacite growth over relict edenitic pargasite in omphacite–bearing jadeitite of the Itoigawa–Omi area of the Hida–Gaien belt, central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390287706350583040","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"LA-ICP-MS zircon U-Pb ages of the Oshima metamorphic complex from Yawatahama-Oshima island and its geotectonic correlation"},{"@language":"ja","@value":"八幡浜大島に分布する大島変成岩体のジルコンU-Pb年代と地体構造上の意義"},{"@language":"ja-Kana","@value":"ヤワタハマ オオシマ ニ ブンプ スル オオシマ ヘンセイガンタイ ノ ジルコン U-Pb ネンダイ ト ジタイ コウゾウ ジョウ ノ イギ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390566775159391872","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Geochemistry and magmatic zircon U–Pb dating of amphibolite blocks in the Omi serpentinite mélange, north central Japan: Possible subduction of the Cambrian oceanic crust"}]},{"@id":"https://cir.nii.ac.jp/crid/1390568456340008832","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A new occurrence of okhotskite in the Kurosegawa belt, Kyushu, Japan: the okhotskite + Mn–lawsonite assemblage as a potential high–pressure indicator"}]},{"@id":"https://cir.nii.ac.jp/crid/1390568456351918464","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Fragments of the early Paleozoic orogenic belt from Tokyo Metropolis, Japan:"},{"@language":"ja","@value":"東京都産古生代前期造山帯の断片："},{"@value":"東京都産古生代前期造山帯の断片 : 関東山地東部,黒瀬川帯高圧型変斑れい岩および花崗岩類のジルコンU-Pb年代"},{"@language":"ja-Kana","@value":"トウキョウトサン コセイダイ ゼンキ ゾウザンタイ ノ ダンペン : カントウ サンチ トウブ,クロセガワタイ コウアツガタ ヘン ハンレイ ガン オヨビ カコウガンルイ ノ ジルコン U-Pb ネンダイ"},{"@value":"Fragments of the early Paleozoic orogenic belt from Tokyo Metropolis, Japan: Zircon U-Pb ages of high P/T-type metagabbro and granitoids of the Kurosegawa belt in eastern Kanto"}]},{"@id":"https://cir.nii.ac.jp/crid/1390584110575770112","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Petrogenesis and U-Pb zircon geochronology of alkali volcanic rocks in the Akiyoshi Terrane, SW Japan and their origin"}]},{"@id":"https://cir.nii.ac.jp/crid/1390853649685822592","@type":"Article","resourceType":"紀要論文(departmental bulletin paper)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Geology of Akiyoshi"}]}],"dataSourceIdentifier":[{"@type":"JALC","@value":"oai:japanlinkcenter.org:2010082756"},{"@type":"CROSSREF","@value":"10.2465/jmps.220630"},{"@type":"KAKEN","@value":"PRODUCT-24597913"},{"@type":"OPENAIRE","@value":"doi_________::716c9dc75c2048c9ab135f56a1c6ca05"},{"@type":"CROSSREF","@value":"10.1002/gj.5052_references_DOI_TuqnvaVglbXxxwZTB3aJO1rT1z1"},{"@type":"CROSSREF","@value":"10.2465/jmps.231222_references_DOI_TuqnvaVglbXxxwZTB3aJO1rT1z1"}]}