{"@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/1360004232498083584.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/j.sedgeo.2011.11.001"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0037073811002661?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0037073811002661?httpAccept=text/plain"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Radiocarbon dating of residual organic matter in travertine formed along the Yumoto Fault in Oga Peninsula, northeast Japan: Implications for long-term hot spring activity under the influence of earthquakes"}],"description":[{"notation":[{"@value":"Abstract   Radiocarbon dating was performed on trace amounts of organic matter included in travertines formed along the Yumoto fault in Oga Peninsula, NE Japan. The reliability of the dating method was confirmed by the consistency of ages obtained with the stratigraphy of the travertine mound and the ratio of carbon stable isotopes. The radiocarbon chronology of the travertines shows that (1) the hot springs at Oga have been active for approximately 29,000 years, with average depositional rates ranging from 0.24 to 1.75 mm/yr, and (2) the principal hot spring activity has migrated southward with time. Variations in the accumulation rates and the progressive migration of the main focus of the hot spring activity imply irregular spring behaviour. This behaviour has not been influenced by paleoclimate, but may have been controlled by the earthquakes that occur frequently in the region around Oga Peninsula."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1420001326226079360","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"90375220"},{"@type":"NRID","@value":"1000090375220"},{"@type":"NRID","@value":"9000243847803"},{"@type":"NRID","@value":"9000365024216"},{"@type":"NRID","@value":"9000392812347"},{"@type":"NRID","@value":"9000005543868"},{"@type":"NRID","@value":"9000005179059"},{"@type":"NRID","@value":"9000006841922"},{"@type":"NRID","@value":"9000024931414"},{"@type":"NRID","@value":"9000005450918"},{"@type":"NRID","@value":"9000286278186"},{"@type":"NRID","@value":"9000414365563"},{"@type":"NRID","@value":"9000010111958"},{"@type":"NRID","@value":"9000409326793"},{"@type":"NRID","@value":"9000020088268"},{"@type":"NRID","@value":"9000409900819"},{"@type":"NRID","@value":"9000254692590"},{"@type":"NRID","@value":"9000258411553"},{"@type":"NRID","@value":"9000242263239"},{"@type":"NRID","@value":"9000004608891"},{"@type":"NRID","@value":"9000347192593"},{"@type":"NRID","@value":"9000248248978"},{"@type":"NRID","@value":"9000018749737"},{"@type":"NRID","@value":"9000020143115"},{"@type":"NRID","@value":"9000018293686"},{"@type":"NRID","@value":"9000350634362"},{"@type":"NRID","@value":"9000254213478"},{"@type":"NRID","@value":"9000403550975"},{"@type":"NRID","@value":"9000255835823"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/nishikawao"}],"foaf:name":[{"@value":"Osamu Nishikawa"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004232498083587","@type":"Researcher","foaf:name":[{"@value":"Kyoko Furuhashi"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004232498083584","@type":"Researcher","foaf:name":[{"@value":"Masashi Masuyama"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004232498083588","@type":"Researcher","foaf:name":[{"@value":"Takeyuki Ogata"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004232498083589","@type":"Researcher","foaf:name":[{"@value":"Tateo Shiraishi"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004232498083586","@type":"Researcher","foaf:name":[{"@value":"Chuan-Chou Shen"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00370738"}],"prism:publicationName":[{"@value":"Sedimentary Geology"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2012-01","prism:volume":"243-244","prism:startingPage":"181","prism:endingPage":"190"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S0037073811002661?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S0037073811002661?httpAccept=text/plain"}],"createdAt":"2011-11-13","modifiedAt":"2018-11-28","project":[{"@id":"https://cir.nii.ac.jp/crid/1040282257150885504","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"23654170"},{"@type":"JGN","@value":"JP23654170"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-23654170/"}],"notation":[{"@language":"ja","@value":"高速進展する断層ラプチャー先端の応力場と破砕現象の解明"},{"@language":"en","@value":"Investigation of stress field and pulverization mechanism at the fault rapture front propagating at a high speed"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360011142931942784","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Bayesian Analysis of Radiocarbon Dates"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011142940225024","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"IntCal09 and Marine09 Radiocarbon Age Calibration Curves, 0–50,000 Years cal BP"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011144278104960","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Radiocarbon Dating of Holocene Calcareous Tufa in Southern Poland"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011144554848512","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Dissected hydrologic system at the Grand Canyon: Interaction between deeply derived fluids and plateau aquifer waters in modern springs and travertine"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011145985044992","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"U/Th dating of freshwater travertine from Middle Velino Valley (Central Italy): paleoclimatic and geological implications"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011146521758976","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Rifting and basin inversion in the eastern margin of the Japan Sea"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285710504507904","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Textures and processes of laminated travertines formed by unicellular cyanobacteria in <scp>M</scp>yoken hot spring, southwestern <scp>J</scp>apan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360290617811355904","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Genesis and diagenesis of travertine, Futamata hot spring, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292619282454016","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Effects of Contamination of Calcareous Sediments on their Radiocarbon Ages"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292621030716672","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Palaeomagnetic and rock magnetic properties of travertine: Its potential as a recorder of geomagnetic palaeosecular variation, environmental change and earthquake activity in the Sıcak Çermik geothermal field, Turkey"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574094333278592","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Studying travertines for neotectonics investigations: Middle–Late Pleistocene syn-tectonic travertine deposition at Serre di Rapolano (Northern Apennines, Italy)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574095308326400","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Radiocarbon Dating of Calcareous Tufa: How Reliable Data can we Expect?"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574095680063104","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Seasonal record from recent fluvial tufa deposits (Monasterio de Piedra, NE Spain): sedimentological and stable isotope data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574096062304256","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Laminated Iron Texture by Iron-Oxidizing Bacteria in a Calcite Travertine"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574096093668096","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The influence of organic material on the polymorphic crystallization of calcium carbonate"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855568499671936","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Reconstruction of Water Temperature, pH, and Flux of Ancient Hot Springs from Travertine Depositional Facies"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855569171625344","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Speleothems, Travertines, and Paleoclimates"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855569283608064","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Depositional Facies and Aqueous-Solid Geochemistry of Travertine-Depositing Hot Springs (Angel Terrace, Mammoth Hot Springs, Yellowstone National Park, U.S.A.)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855569558198912","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Climate-induced changes in Holocene calcareous tufa formations, Bohemian Karst, Czech Republic"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137045979470976","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Problem of Palaeokarst in Tibet"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418518503853568","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The quaternary travertine deposits of Europe and Asia Minor"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418521164878592","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Earthquakes, strain-cycling and the mobilization of fluids"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699993432720128","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Origin of annual laminations in tufa deposits, southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699995517257728","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Calculation of Past Dead Carbon Proportion and Variability by the Comparison of AMS <sup>14</sup>C and Tims U/TH Ages on Two Holocene Stalagmites"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981468715008512","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Vegetation and Climate during the Last Glacial Maximum in Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981469313281024","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Factors controlling present-day tufa dynamics in the Monasterio de Piedra Natural Park (Iberian Range, Spain): depositional environmental settings, sedimentation rates and hydrochemistry"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262944293892096","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"U-series dating and geochemical tracing of late Quaternary travertine in co-seismic fissures"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262945052384384","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Warm Period Growth of Travertine during the Last Interglaciation in Southern Germany"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262945754279936","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Travitonics: using travertines in active fault studies"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262945857866112","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Discussion Reporting of <sup>14</sup>C Data"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262946105382400","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Late Pleistocene depositional cycles of the Lapis Tiburtinus travertine (Tivoli, Central Italy): Possible influence of climate and fault activity"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544418658343552","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Tufas and travertines of the Mediterranean region: a testing ground for freshwater carbonate concepts and developments"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825893793319296","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Calcified microbial mats date prehistoric canals—Radiocarbon assay of organic extracts from travertine"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825894678189568","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Travertine deposition and faulting: the fault-related travertine fissure-ridge at Terme S. Giovanni, Rapolano Terme (Italy)"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825894820843392","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Hot‐spring Systems Geobiology: abiotic and biotic influences on travertine formation at Mammoth Hot Springs, Yellowstone National Park, USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825895734024448","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Preferential soft-tissue preservation in the Hot Creek carbonate spring deposit, British Columbia, Canada"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107369558215808","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Sedimentary patterns in perched spring travertines near Granada (Spain) as indicators of the paleohydrological and paleoclimatological evolution of a karst massif"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107369982947456","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A review of tufa and travertine deposits of the world"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107370608859392","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Relationship between tectonics, volcanism, sedimentation and basin development, Late Cenozoic, central part of Northern Honshu, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388843578521088","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Travertine deposits from along the South Tibetan Fault System near Nyalam, Tibet"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388844415280128","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Differences in the 14C age, δ13C and δ18O of Holocene tufa and speleothem in the Dinaric Karst"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388845742083328","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Deposition and diagenesis of Mammoth Hot Springs travertine, Yellowstone National Park, Wyoming, U.S.A."}]},{"@id":"https://cir.nii.ac.jp/crid/1363951795524691072","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Factors controlling growth of modern tufa: results of a field experiment"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951795538261376","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Holocene environmental changes in Lake Bangong basin (Western Tibet). Part 1: Chronology and stable isotopes of carbonates of a Holocene lacustrine core"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233268323714560","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Radiocarbon Dating of Tufa in Paleoclimatic Studies"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233268644681344","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Hot‐spring travertine facies and sequences, Late Pleistocene, Rapolano Terme, Italy"}]},{"@id":"https://cir.nii.ac.jp/crid/1371132819166732416","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Radiocarbon chronology of carbonate deposits—reliable dating using organic residues. Abstracts with Programs"}]},{"@id":"https://cir.nii.ac.jp/crid/1371132819166732422","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Geochemistry of calcareous deposits found in hot springs"}]},{"@id":"https://cir.nii.ac.jp/crid/1371132819166732547","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Isotope and geochemical study of travertine and hot springs occurring along the Yumoto fault at the north coast of the Oga Peninsula, Akita Prefecture"}]},{"@id":"https://cir.nii.ac.jp/crid/1371132819166732674","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Accelerator and radiometric radiocarbon dates on a range of materials from colluvial deposits from Holywell Coombe, Folkestone"}]},{"@id":"https://cir.nii.ac.jp/crid/1371132819166732684","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Explanatory map of the geological map of Japan: Toga and Funakawa sheets (scale 1:50,000)"}]},{"@id":"https://cir.nii.ac.jp/crid/1371132819166732686","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The geology of the Ogashima oil field, Prefecture of Akita"}]},{"@id":"https://cir.nii.ac.jp/crid/1371132819166732687","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Seasonal variations of hydrochemistry and carbonate precipitation rate in a travertine-depositing canal at Baishuitai, Yunnan, SW China: implications for the formation of biannual laminae in travertine and climatic reconstruction"}]},{"@id":"https://cir.nii.ac.jp/crid/1371132819166732692","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Iriai Formation: a newly defined marine terrace deposit correlative with oxygen isotope stage 5a in the Oga Peninsula, Akita Prefecture, Northeast Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1371132819166732695","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Volcanic facies in the Oga Peninsula: Eocene to Early Miocene volcanic rocks and Toga volcano"}]},{"@id":"https://cir.nii.ac.jp/crid/1371132819166732808","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Compilation of thermal gradient data in Japan on the basis of the temperatures in boreholes"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206238500992","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Depositional processes of travertine developed at Shionoha hot spring, Nara Prefecture, Japan"},{"@language":"ja","@value":"奈良県入之波温泉に発達するトラバーチンの堆積過程"},{"@language":"ja-Kana","@value":"ナラケン シオノハ オンセン ニ ハッタツ スル トラバーチン ノ タイセキ カテイ"},{"@value":"Depositional process of travertine developed at Shionoha hot spring, Nara Prefecture, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206240523904","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Geomorphology and Quaternary geology of the Oga-Noshiro area, Akita Prefecture"},{"@language":"ja","@value":"男鹿半島－能代地域の地形と第四系"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1016/j.sedgeo.2011.11.001"},{"@type":"KAKEN","@value":"PRODUCT-14243830"},{"@type":"KAKEN","@value":"PRODUCT-14243825"},{"@type":"OPENAIRE","@value":"doi_dedup___::7825e0e221a16104530c704ae4fa08df"},{"@type":"CROSSREF","@value":"10.1111/iar.12034_references_DOI_BDOVggcNB8AEyNfcYaUTay2xT0q"},{"@type":"CROSSREF","@value":"10.1016/j.sedgeo.2020.105706_references_DOI_BDOVggcNB8AEyNfcYaUTay2xT0q"}]}