{"@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/1362262945859196160.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/0031-0182(92)90060-i"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:003101829290060I?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:003101829290060I?httpAccept=text/plain"}}],"dc:title":[{"@value":"Jurassic-Early cretaceous tectonic evolution of the Southern Chichibu terrane, southwest Japan"}],"description":[{"notation":[{"@value":"Abstract   The Southern Chichibu terrane fringes the southern margin of the Jurassic-Early Cretaceous accretionary complex of southwest Japan. Two subterranes, the Togano subterrane in the north and Sambosan subterrane to the south, are recognized by examination of the common features of the terrane. They are juxtaposed throughout the terrane from western Kyushu to the Kanto Mountains a distance of over 1000 km. The geology of the Sakawa area, central Shikoku, is described in detail to show an example of the terrane. The geology around Tsukumi in eastern Kyushi and Okutama in the Kanto Mountains is introduced to emphasize the common features of this terrane.  The Togano subterrane is composed of predominantly Triassic-Jurassic chert-clastic sequences with subordinate Jurassic olistostromal sequences and Upper Jurassic-Lower Cretaceous limestone-bearing clastic sequences. The chert-clastic sequences show an upward-coarsening sequence which reflects landward drift of the sea floor from a pelagic realm towards a trench. The olistostromal sequence contains abundant upper Paleozoic blocks. This subterrane is characterized by a south-vergent imbricate structure and south-younging polarity of the chert-clastic sequences.  The Sambosan subterrane consists of mainly Upper Jurassic-Lower Cretaceous olistostromal sequences associated with Upper Jurassic-Lower Cretaceous limestone-bearing clastic sequences. The olistostromal sequence includes abundant Triassic-Jurassic chert blocks and Triassic limestone blocks accompanied by greenstones. The limestone-bearing clastic sequences of both subterranes are regarded as shelf or inner-trench slope sediments on the chert-clastic and olistostromal sequences.  Two major stages of tectonic development are discriminated. The Togano subterrane was formed by successive offscrape-accretion mainly during the Middle to Late Jurassic. The Sambosan subterrane was constructed by collision-accretion of seamounts mainly during the Late Jurassic to Early Cretaceous. The difference in the tectonic processes is considered to relate to topography of subducting oceanic plate; an oceanic plate with an abyssal plain for the Togano subterrane and an oceanic plate with seamounts for the Sambosan subterrane."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1382262945859196160","@type":"Researcher","foaf:name":[{"@value":"Atsushi Matsuoka"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00310182"}],"prism:publicationName":[{"@value":"Palaeogeography, Palaeoclimatology, Palaeoecology"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"1992-10","prism:volume":"96","prism:number":"1-2","prism:startingPage":"71","prism:endingPage":"88"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:003101829290060I?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:003101829290060I?httpAccept=text/plain"}],"createdAt":"2003-08-07","modifiedAt":"2019-03-15","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050282813184366848","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Complex microseismic activity and depth-dependent stress field changes in Wakayama, southwestern Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002215912284288","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Large deep-seated landslides controlled by geologic structures: Prehistoric and modern examples in a Jurassic subduction–accretion complex on the Kii Peninsula, central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002215942228352","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Recognizing OIB and MORB in accretionary complexes: A new approach based on ocean plate stratigraphy, petrology and geochemistry"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232324559488","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Strontium and carbon isotope stratigraphy of the Late Jurassic shallow marine limestone in western Palaeo-Pacific, northwest Borneo"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004235527837568","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Carbon isotope stratigraphy of <scp>T</scp>orinosu‐type limestone in the western <scp>P</scp>aleo‐<scp>P</scp>acific and its implication to paleoceanography in the <scp>L</scp>ate <scp>J</scp>urassic and earliest <scp>C</scp>retaceous"}]},{"@id":"https://cir.nii.ac.jp/crid/1360005516833181952","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Distribution of gravitational slope deformation and deep-seated landslides controlled by thrust faults in the Shimanto accretionary complex"}]},{"@id":"https://cir.nii.ac.jp/crid/1360009142615621248","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Birth and death of seamounts in the Panthalassa Ocean: Late Triassic to Early Jurassic sedimentary record at Mount Sambosan, Shikoku, Southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360016978969523072","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Middle Miocene forearc alkaline magmatism in Amami-Oshima Island, central Ryukyu Arc: implications for paleoreconstruction of Shikoku Basin"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285710504538752","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"<scp>L</scp>ate <scp>T</scp>riassic ammonoid <i><scp>S</scp>irenites</i> from the <scp>S</scp>abudani <scp>F</scp>ormation in <scp>T</scp>okushima, <scp>S</scp>outhwest <scp>J</scp>apan, and its biostratigraphic and paleobiogeographic implications"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285710504940160","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Lithology and radiolarian age of the Ryokami‐yama Chert Formation in eastern Mt. 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Complex, Shikoku Island, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657350076032","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Sedimentary PGE signatures in the Late Triassic ejecta deposits from Japan: Implications for the identification of impactor"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657350099328","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Paleoecology, biogeography, and evolution of reef ecosystems in the Panthalassa Ocean during the Late Triassic: Insights from reef limestone of the Sambosan Accretionary Complex, Shikoku, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865816790695552","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Origin of Alkaline Basaltic Intrusive Rocks in an Exhumed Accretionary Complex: 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Japan"},{"@language":"ja","@value":"高知県佐川地域の七良谷層から最上部ジュラ系アンモノイドの産出"},{"@language":"ja-Kana","@value":"コウチケンサガワ チイキ ノ ナナ リョウダニソウ カラ サイ ジョウブ ジュラケイ アンモノイド ノ サンシュツ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206241475328","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Coniform conodonts collected from the Aso limestone body in the Chichibu Belt, Mie Prefecture"},{"@language":"ja","@value":"三重県秩父帯阿曽カルストの石灰岩体から産出した円錐状コノドント"},{"@language":"ja-Kana","@value":"ミエケン チチブタイアソカルスト ノ セッカイガンタイ カラ サンシュツ シタ エンスイジョウ コノドント"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206241926912","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Stratigraphy and radiolarian ages of stratiform manganese deposits from the Chichibu Belt in the Saiki area, eastern Oita Prefecture, Japan"},{"@language":"ja","@value":"大分県東部佐伯地域の秩父帯に産する層状マンガン鉱床の層序と放散虫化石年代"},{"@language":"ja-Kana","@value":"オオイタケン トウブ サエキ チイキ ノ チチブタイ ニ サンスル ソウジョウ マンガン コウショウ ノ ソウ ジョ ト ホウサンチュウ カセキ ネンダイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679064619392","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Late Triassic bivalves from Sambosan accretionary complex, southwest Japan, and their biogeographic implications"},{"@value":"Late Triassic bivalves from the Sambosan accretionary complex, Southwest Japan, and their biogeographic implications"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681213756800","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Upper Triassic reefal limestone from the Sambosan accretionary complex in Japan and its geological implication"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681214098176","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Megafossil-bearing mudstone blocks in the Oriai Formation of the Upper Jurassic Imaidani Group in the Shirokawa area, Ehime Prefecture, Southwest Japan"},{"@language":"ja","@value":"愛媛県城川地域に分布する上部ジュラ系今井谷層群下相層中の含大型化石泥質岩岩塊"},{"@language":"ja-Kana","@value":"エヒメケンシロカワ チイキ ニ ブンプ スル ジョウブ ジュラケイ イマイダニソウグン カソウソウ チュウ ノ ガン オオガタ カセキ デイシツガン ガンカイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681214217728","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The Inumodorikyo Complex of the Southern Chichibu Belt in the eastern Kii Peninsula, Southwest Japan: radiolarian ages and the Nomata Thrust"},{"@language":"ja","@value":"紀伊半島東部秩父南帯の犬戻峡コンプレックス：放散虫化石年代と野又衝上断層"},{"@language":"ja-Kana","@value":"キイ ハントウ トウブ チチブ ナンタイ ノ イヌモドリキョウ コンプレックス ホウサンチュウ カセキ ネンダイ ト ノマタ ショウジョウ ダンソウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681214475904","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Origin of basalts from Sambosan accretionary complex, Shikoku and Kyushu"},{"@language":"ja","@value":"九州・四国の三宝山付加コンプレックスの玄武岩類の起源"},{"@value":"九州・四国三宝山付加コンプレックスの玄武岩類の起源"},{"@language":"ja-Kana","@value":"キュウシュウ シコク サンボウサン フカ コンプレックス ノ ゲンブガンルイ ノ キゲン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681214534912","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Strontium isotopic age of the Torinosu Limestone in Niyodo Village, Kochi Prefecture, SW Japan."},{"@language":"ja","@value":"高知県仁淀村に分布する鳥巣石灰岩のストロンチウム同位体年代"},{"@language":"ja-Kana","@value":"コウチケン ニヨドムラ ニ ブンプ スル トリノス セッカイガン ノ ストロンチウム ドウイタイ ネンダイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681216094976","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Jurassic accretionary complex and trench-slope deposits in western Kyushu, Japan"},{"@language":"ja","@value":"九州西部に分布するジュラ紀付加体と海溝斜面堆積物"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282763104089216","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Recent progress in Paleozoic-Mesozoic microfossil research in deep-sea sediments of Japanese accretionary complexes:"},{"@language":"ja","@value":"付加体深海堆積相における中・古生代微化石研究の最近の進展："},{"@value":"付加体深海堆積相における中・古生代微化石研究の最近の進展 : 放散虫およびコノドント研究の現状と将来の展望"},{"@language":"ja-Kana","@value":"フカタイ シンカイ タイセキソウ ニ オケル ナカ ・ コセイダイ ビカセキ ケンキュウ ノ サイキン ノ シンテン : ホウサンチュウ オヨビ コノドント ケンキュウ ノ ゲンジョウ ト ショウライ ノ テンボウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282763133774464","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Geological structure and detrital zircon U-Pb age around 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