{"@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/1360848656243199744.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1007/s10347-016-0475-7"}},{"identifier":{"@type":"URI","@value":"http://link.springer.com/content/pdf/10.1007/s10347-016-0475-7.pdf"}},{"identifier":{"@type":"URI","@value":"http://link.springer.com/article/10.1007/s10347-016-0475-7/fulltext.html"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Mid-oceanic shallow-water carbonates of the Panthalassa domain: new microfacies data from the Sambosan Accretionary Complex, Shikoku Island, Japan"}],"description":[{"notation":[{"@value":"During the Late Triassic, carbonate platforms expanded on continental shelves and island arcs. They have been studied in detail in the Tethys realm but coeval mid-oceanic shallow-water environments of the Panthalassa domain have received less attention. To fill this gap, we investigated the Upper Triassic limestone of the Sambosan Accretionary Complex (SAC), southwest Japan. A comprehensive sampling of the Upper Triassic limestone has been performed in 16 localities at Shikoku Island. Eight microfacies, ranging from pelagic to lagoonal settings, were identified, including two microfacies that are described in the SAC for the first time. Quantitative microfacies analysis assesses the composition of the SAC limestone and its biostratigraphy is refined. Finally, a speculative depositional model of the SAC carbonate platforms is proposed based on modern and ancient analogues. Instead of a true atoll-type platform with well-defined facies belts as suggested by previous studies, this new model suggests that the typical Sambosan platform was more probably a carbonate bank with submerged margins and a mosaic of microfacies in the platform interior. Special attention is given to the factors that have probably controlled the carbonate sedimentation at the top of the seamount(s)."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380848656243199234","@type":"Researcher","foaf:name":[{"@value":"C. Peybernes"}]},{"@id":"https://cir.nii.ac.jp/crid/1380848656243199241","@type":"Researcher","foaf:name":[{"@value":"J. Chablais"}]},{"@id":"https://cir.nii.ac.jp/crid/1380848656243199752","@type":"Researcher","foaf:name":[{"@value":"T. Onoue"}]},{"@id":"https://cir.nii.ac.jp/crid/1380848656243199490","@type":"Researcher","foaf:name":[{"@value":"R. Martini"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01729179"},{"@type":"EISSN","@value":"16124820"}],"prism:publicationName":[{"@value":"Facies"}],"dc:publisher":[{"@value":"Springer Science and Business Media LLC"}],"prism:publicationDate":"2016-08-05","prism:volume":"62","prism:number":"4"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["http://www.springer.com/tdm"],"url":[{"@id":"http://link.springer.com/content/pdf/10.1007/s10347-016-0475-7.pdf"},{"@id":"http://link.springer.com/article/10.1007/s10347-016-0475-7/fulltext.html"}],"createdAt":"2016-08-05","modifiedAt":"2022-07-05","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=Sambosan%20Accretionary%20Complex","dc:title":"Sambosan Accretionary Complex"},{"@id":"https://cir.nii.ac.jp/all?q=info:eu-repo/classification/ddc/550","dc:title":"info:eu-repo/classification/ddc/550"},{"@id":"https://cir.nii.ac.jp/all?q=Microfacies","dc:title":"Microfacies"},{"@id":"https://cir.nii.ac.jp/all?q=Panthalassa","dc:title":"Panthalassa"},{"@id":"https://cir.nii.ac.jp/all?q=Shallow-water%20carbonates","dc:title":"Shallow-water carbonates"},{"@id":"https://cir.nii.ac.jp/all?q=Seamount","dc:title":"Seamount"},{"@id":"https://cir.nii.ac.jp/all?q=Japan","dc:title":"Japan"},{"@id":"https://cir.nii.ac.jp/all?q=Upper%20Triassic","dc:title":"Upper Triassic"}],"project":[{"@id":"https://cir.nii.ac.jp/crid/1040000781825267712","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"15H02142"},{"@type":"JGN","@value":"JP15H02142"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-15H02142/"}],"notation":[{"@language":"ja","@value":"顕生代の海水オスミウム同位体変動から読み解く地球表層環境変遷"},{"@language":"en","@value":"Environmental change elucidated from seawater Os isotope in Phanerozoic"}]},{"@id":"https://cir.nii.ac.jp/crid/1040000782482916736","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"15H05771"},{"@type":"JGN","@value":"JP15H05771"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-15H05771/"}],"notation":[{"@language":"ja","@value":"海の鉱物資源の科学と工学の新展開"},{"@language":"en","@value":"New developments in science and engineering of mineral resources from present and past oceans"}]},{"@id":"https://cir.nii.ac.jp/crid/1040282257290699520","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"26707027"},{"@type":"JGN","@value":"JP26707027"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-26707027/"}],"notation":[{"@language":"ja","@value":"中・古生代層状チャートに記録された隕石衝突履歴の完全解読"},{"@language":"en","@value":"Search for evidence of impact in the Paleozoic and Mesozoic bedded cherts in Japan"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360002215942228352","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"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/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/1360011143534903424","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Cretaceous Drowning of Reefs on Mid-Pacific and Japanese Guyots"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011143927900672","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Ocean Plate Stratigraphy in East and Southeast Asia"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011144270405504","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Sequence stratigraphy after the demise of a high-relief carbonate platform (Carnian of the Dolomites): Sea-level and climate disentangled"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011145107845632","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Norian-Rhaetian reefs in Argolis Peninsula, Greece"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011145187435264","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Giant Submarine Alika Debris Slide, Mauna Loa, Hawaii"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011145927883776","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Paläontologie, Fazies und Geochemie der Dachstein-Kalke (Ober-Trias) im südwestlichen Gesäuse, Steiermark, Österreich"}]},{"@id":"https://cir.nii.ac.jp/crid/1360017280653784832","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Sedimentology and biostratigraphy of the upper <scp>Triassic</scp> carbonates from the <scp>Shiriya</scp> cape, <scp>North Kitakami Belt, Japan</scp>"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285715191099648","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Temporal changes in biotic and abiotic composition of shallow-water carbonates on submerged seamounts in the northwestern Pacific Ocean and their controlling factors"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292618492468096","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Microboring and taphonomy in Middle Oxfordian to lowermost Kimmeridgian (Upper Jurassic) from the Prebetic Zone (southern Iberia)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292618856804864","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Foraminifera and their associations of a possibly Rhaetian section of the Nayband Formation in central Iran, northeast of Esfahan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292618988949760","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Microfacies and depositional setting of the Upper Triassic mid-oceanic atoll-type carbonates of the Sambosan Accretionary Complex (southern Kyushu, Japan)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292619031291008","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Upper Triassic, Dachstein-Type, Reef Limestone from the Wallowa Mountains, Oregon: First Reported Occurrence in the United States"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292619053473152","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The changing climate framework and depositional dynamics of Triassic carbonate platforms from the Dolomites"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292620389142528","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Climate of the Supercontinent Pangea"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292620952818944","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Climate-induced fluctuations in sea level during non-glacial times"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565165997882240","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Oceanic island basalts in accretionary complexes of SW Japan: Tectonic and petrogenetic implications"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574094453141376","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Sedimentation on Rasdhoo and Ari Atolls, Maldives, Indian Ocean"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574094528415616","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The endo-upwelling concept: from geothermal convection to reef construction"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574094612583424","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Modern foraminiferal distribution and diversity in two atolls from the Maldives, Indian Ocean"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574094850764288","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Submarine Landslides in French Polynesia"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574094977098240","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Upper Triassic carbonate deposits of Seram (Indonesia): palaeogeographic and geodynamic implications"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574095039137152","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Depth transect of an Upper Triassic (Rhaetian) reef from Gosau, Austria: Microfacies and community ecology"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574095613165568","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Side‐scan sonar images of submarine landslides on the flanks of atolls and guyots"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574095747270272","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Lofer cyclothems revisited (Late triassic, Northern Alps, Austria)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574095849180416","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Upper Triassic (Ladinian?-Carnian) reef biota from the Sambosan Accretionary Complex, Shikoku, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574096190278528","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Nouvelle classificationdes Foraminifères Endothyroïdes du Trias"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574096503231360","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Problems with reef models: The late triassic steinplatte “Reef” (Northern Alps, Salzburg/Tyrol, Austria)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360579816412557952","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Upper Triassic foraminifers from Panthalassan carbonate buildups of Southwestern Japan and their paleobiogeographic implications"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657350099328","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"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/1360855568548319872","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Facies, geometry and growth phases of the Valdorria carbonate platform (Pennsylvanian, northern Spain)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855568618954624","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Holocene Sediment Types and Their Distribution in the Southern Persian Gulf"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855569014033280","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Microbial boundstone dominated carbonate slope (Upper Carboniferous, N Spain): Microfacies, lithofacies distribution and stratal geometry"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855570006684672","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The role of oblique subduction and strike-slip tectonics in the evolution of Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855570019080064","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Depositional response to the Late Triassic ascent of calcareous plankton in pelagic mid-oceanic plate deposits of Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855570187158144","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Upper Triassic platform margin biofacies and the paleogeography of Southern Apennines"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137043566182528","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Quantification of input and compositional variations of calciturbidites in a Middle Triassic basinal succession (Seceda, Dolomites, Southern Alps)"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137044252474368","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"<i>Aulotortus friedli</i>from the Upper Triassic Gravitational Flow Deposits of the Kumagawa River (Kyushu, Southwest Japan)"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137044410944512","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The reefal margin and slope of a Middle Triassic carbonate platform: the Latemar (Dolomites, Italy)"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137045173258496","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Carboniferous reef succession of the Panthalassan open-ocean setting: example from Omi Limestone, central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418519192945280","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"TRIASSIC SEA-LEVEL CHANGES: EVIDENCE FROM THE CANADIAN ARCTIC ARCHIPELAGO"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418519380875392","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"New crustacean microcoprolites of the Upper Triassic limestones of the Sambosan Accretionary Complex, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418519827850240","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Facies of sunken early cretaceous atoll reefs and their capping Late Albian drowning succession (Northwestern Pacific)"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418521026588288","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Facies architecture of an isolated carbonate platform: tracing the cycles of the Latemàr (Middle Triassic, northern Italy)"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699994152614400","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Anatomy and genesis of a subduction‐related orogen: A new view of geotectonic subdivision and evolution of the Japanese Islands"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699994780376704","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"TAPHONOMIC FEATURES OF LATE TRIASSIC FORAMINIFERA FROM MOUNT BEGUNJ  ICA, KARAVANKE MOUNTAINS, SLOVENIA"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699995029424768","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"CENOZOIC PROGRADATION OF NORTHWESTERN GREAT BAHAMA BANK, A RECORD OF LATERAL PLATFORM GROWTH AND SEA-LEVEL FLUCTUATIONS"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699995437544576","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"“Oman Exotics”—Oceanic carbonate build-ups associated with the early stages of continental rifting"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981468871169024","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"New model for the Early Cretaceous development of SW Japan based on basic rocks of the Chichibu Composite Terrane"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981468915553024","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Seismic stratigraphy of the Frontal Hawaiian Moat: implications for sedimentary processes at the leading edge of an oceanic hotspot trace"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981470781871488","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Sedimentology, stratigraphy, and micropalaeontology of the Upper Triassic reefal series in Eastern Sulawesi (Indonesia)"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981471362654848","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Recent sedimentary facies of isolated carbonate platforms, Belize-Yucatan system, Central America"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262944352193024","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Upper Triassic reefs of the Oman Mountains: Data from the South Tethyan margin"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262944704986368","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Fazielle Entwicklung und Palökologische Zonierung Zweier Obertriadischer Riffstrukturen in den Nördlichen Kalkalpen (“Oberrhät”-Riff-Kalke, Salzburg)"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262945125362176","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Mikrofazies, Paläontologie und Palökologie der Dachsteinriffkalke (Nor) des Gosaukammes, Österreich"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262945859196160","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Jurassic-Early cretaceous tectonic evolution of the Southern Chichibu terrane, southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544418512681984","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Sedimentary facies from Upper Triassic reefal limestone of the Sambosan accretionary complex in Japan: mid-ocean patch reef development in the Panthalassa Ocean"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544418630751232","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Quantitative compositional analysis of a Triassic carbonate platform (Southern Alps, Italy)"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544419100003200","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Causal or casual link between the rise of nannoplankton calcification and a tectonically-driven massive decrease in Late Triassic atmospheric CO2?"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544419445993984","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Late paleozoic and Late Triassic limestones from north Palawan Block (Philippines): Microfacies and paleogeographical implications"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825893256326272","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Geological History of Deep-Sea Volcanoes: Biosphere, Hydrosphere, and Lithosphere Interactions"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825894228096768","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Significance of \"Tethyan\" Fossils in the American Cordillera"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825894729664256","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Developing a strategy for accurate definition of a geological boundary through radio-isotopic and biochronological dating: The Early–Middle Triassic boundary (South China)"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825894782711424","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Chronology of Fluctuating Sea Levels Since the Triassic"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825895670135168","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Triassic mid‐oceanic sedimentation in Panthalassa Ocean: Sambosan accretionary complex, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825895926940032","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Nature and evolution of Middle Triassic carbonate buildups in the Dolomites (Italy)"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107368310931968","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Gulf: Facies Belts, Physical, Chemical, and Biological Parameters of Sedimentation on a Carbonate Ramp"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107368832373888","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Upper Triassic reef-limestone blocks of southwestern Japan: New data from a Panthalassan seamount"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107369392146688","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Triassic Foraminifers from Sites 761 and 764, Wombat Plateau, Northwest Australia"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107369420996608","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Mappable features of mélanges derived from Ocean Plate Stratigraphy in the Jurassic accretionary complexes of Mino and Chichibu terranes in Southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107370369364352","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Carbonate Sedimentology"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388844533952512","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Phanerozoic Record of Global Sea-Level Change"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388844654675200","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Rudist bivalves and the Pacific in the Late Jurassic and Early Cretaceous"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388844693891328","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Quaternary reef response to sea‐level and environmental change in the western Atlantic"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388846182534144","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Windward-leeward effects on Triassic carbonate bank margin facies of the Dolomites, northern Italy"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670318934459904","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Triassic climates — State of the art and perspectives"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670320032202368","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"EARLY EVOLUTION AND NEW CLASSIFICATION OF THE ORDER ROBERTINIDA (FORAMINIFERA)"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670320286347136","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Prodigious submarine landslides on the Hawaiian Ridge"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951793842934656","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Latemar: A flat-topped, steep fronted platform dominated by microbialites and synsedimentary cements"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951793977978496","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Towards accurate numerical calibration of the Late Triassic: High-precision U-Pb geochronology constraints on the duration of the Rhaetian"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951794613456128","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Mapping bathymetry and depositional facies on Great Bahama Bank"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951795373828608","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Oligocene sea-level falls recorded in mid-Pacific atoll and archipelagic apron settings"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951796250649344","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Shelf-to-basin facies distributions and sequence stratigraphy of a steep-rimmed carbonate margin; Capitan depositional system, McKittrick Canyon, New Mexico and Texas"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233269157207680","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Mesozoic climates: General circulation models and the rock record"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233269247330560","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Microbial controls on Panthalassan Carboniferous-Permian oceanic Buildups, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233269368649344","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"An upper Tuvalian (Triassic) platform-basin system in the Julian Alps: the start-up of the Dolomia Principale (Southern Alps, Italy)"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233269593898240","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Facies architecture of an isolated carbonate platform in the Hawasina Basin: The Late Triassic Jebel Kawr of Oman"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233270641286016","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Platy coral patch reefs from eastern Panthalassa (Nevada, USA): Unique reef construction in the Late Triassic"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233270970440832","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Calciturbidite composition related to exposure and flooding of a carbonate platform (Triassic, Eastern Alps)"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233271130564736","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Offshore evidence for a huge landslide of the northern flank of Tahiti‐Nui (French Polynesia)"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206237402368","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Geological history of the Yabe guyot to the east of the Ogasawara Islands"},{"@value":"小笠原諸島東方,矢部海山(新称)の地史"},{"@language":"ja-Kana","@value":"オガサワラ ショトウ トウホウ ヤベ ウミヤマ シンショウ ノ チシ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206238197760","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Origin and metamorphism of greenstones from the Sanbosan unit of the Southern Chichibu Belt, west to central east Shikoku"},{"@value":"四国西部～中東部の南部秩父帯三宝山ユニットに分布する緑色岩類の起源と変成作用"},{"@language":"ja-Kana","@value":"シコク セイブ チュウトウブ ノ ナンブ チチブタイ サンボウサン ユニット ニ ブンプ スル リョクショクガンルイ ノ キゲン ト ヘンセイ サヨウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206240595200","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Stratigraphy and conodont and ammonoid ages of Upper Triassic Nakijin Formation in Hedomisaki area, Okinawa-jima, Japan"},{"@language":"ja","@value":"沖縄県辺戸岬，上部三畳系今帰仁層の岩相層序とコノドントおよびアンモナイト化石年代"},{"@language":"ja-Kana","@value":"オキナワケン ヘンドミサキ,ジョウブ サンジョウケイ コンキジンソウ ノ ガンソウソウ ジョ ト コノドント オヨビ アンモナイト カセキ ネンダイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206240940672","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Reexamination of the Palaeozoic and Mesozoic formations in the Southern Zone of the Chichibu Belt in eastern Shikoku by means of conodonts and fusulinids"},{"@value":"四国東部の秩父累帯南帯中・古生界層序のコノドントと紡錘虫による再検討"},{"@language":"ja-Kana","@value":"シコク トウブ ノ チチブ ルイタイ ナンタイチュウ コセイカイ ソウジョ ノ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679064619392","@type":"Article","relationType":["references"],"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/1390282681210221952","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Research progress in the Chichibu Composite Belt-Reports from western Shikoku. Unit division for the Chichibu Composite Belt from a view point of accretionary tectonics and geology of western Shikoku, Japan."},{"@value":"秩父累帯研究の新展開　　四国西部からの発信　　付加体地質の観点に立った秩父累帯のユニット区分と四国西部の地質"},{"@language":"ja-Kana","@value":"フカタイ チシツ ノ カンテン ニ タッタ チチブルイタイ ノ ユニット クブ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681213424256","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Difference between the Kochigatani and Tethyan bivalve faunas in the Late Triassic of Japan and its implication."},{"@value":"後期三畳紀の河内ケ谷二枚貝化石群とテチス二枚貝化石群の対立とその意義"},{"@language":"ja-Kana","@value":"コウキ 3ジョウキ ノ コウチガタニ 2マイ カイ カセキグン ト テチス 2"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681213756800","@type":"Article","relationType":["references"],"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/1390282681214475904","@type":"Article","relationType":["references"],"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/1390282681214490240","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Tectonic division of the Chichibu Composite-terrane in the westernmost part of Shikoku, southwest Japan"},{"@value":"四国西端部秩父累帯の地体構造区分"},{"@language":"ja-Kana","@value":"シコク セイタンブ チチブルイタイ ノ チタイ コウゾウ クブン"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1007/s10347-016-0475-7"},{"@type":"KAKEN","@value":"PRODUCT-20779146"},{"@type":"KAKEN","@value":"PRODUCT-20764590"},{"@type":"KAKEN","@value":"PRODUCT-21039455"},{"@type":"OPENAIRE","@value":"doi_dedup___::62a2fb32a54aa8d63631719e1aca5cba"},{"@type":"CROSSREF","@value":"10.1016/j.gloplacha.2020.103250_references_DOI_Xp6lBF0mPXIUb43gJm5NYYQ3RYD"},{"@type":"CROSSREF","@value":"10.1111/iar.12473_references_DOI_Xp6lBF0mPXIUb43gJm5NYYQ3RYD"}]}