{"@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/1362825895121024384.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1017/s0033822200057908"}},{"identifier":{"@type":"URI","@value":"https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033822200057908"}}],"dc:title":[{"@value":"Age Determination of the Kawagodaira Volcanic Eruption in Japan by <sup>14</sup>C Wiggle-Matching"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>The Kawagodaira Volcano is located on the northwest slope of Amagi Volcano on the Izu Peninsula of central Japan. The fine pumice that erupted from Kawagodaira Volcano is widely distributed in the central and western parts of the Japanese mainland. Here, we report an accurate eruption age determined by radiocarbon wiggle-matching of a Japanese cedar timber excavated from the pyroclastic deposit at the pumice flow terminal of Kawagodaira Volcano. The <jats:sup>14</jats:sup>C wiggle-match estimate for the Kawagodaira Volcano eruption is 1210–1187 cal BC (95.4% confidence level).</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1382825895121024386","@type":"Researcher","foaf:name":[{"@value":"Sayaka Tani"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895121024388","@type":"Researcher","foaf:name":[{"@value":"Hiroyuki Kitagawa"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895121024384","@type":"Researcher","foaf:name":[{"@value":"Wan Hong"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895121024389","@type":"Researcher","foaf:name":[{"@value":"Jung Hun Park"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895121024387","@type":"Researcher","foaf:name":[{"@value":"Ki Suk Sung"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895121024385","@type":"Researcher","foaf:name":[{"@value":"Gyujun Park"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00338222"},{"@type":"EISSN","@value":"19455755"}],"prism:publicationName":[{"@value":"Radiocarbon"}],"dc:publisher":[{"@value":"Cambridge University Press (CUP)"}],"prism:publicationDate":"2013","prism:volume":"55","prism:number":"2","prism:startingPage":"748","prism:endingPage":"752"},"reviewed":"false","dc:rights":["https://www.cambridge.org/core/terms"],"url":[{"@id":"https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033822200057908"}],"createdAt":"2017-01-20","modifiedAt":"2019-04-24","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050282813846346112","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Examination of the largest-possible tsunamis (Level 2) generated along the Nankai and Suruga troughs during the past 4000years based on studies of tsunami deposits from the 2011 Tohoku-oki tsunami"},{"@value":"Examination of the largest-possible tsunamis (Level 2 tsunami) generated along the Nankai and Suruga troughs during the past 4000 years based on studies of tsunami deposits from the 2011 Tohoku-oki tsunami"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283691114260096","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Integrating the Holocene tephrostratigraphy for East Asia using a high-resolution cryptotephra study from Lake Suigetsu (SG14 core), central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360306505602437760","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Development of an automated extraction and radiocarbon dating method for fossil pollen deposited in lake Motosu, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182422877312","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Mt. Fuji Holocene eruption history reconstructed from proximal lake sediments and high-density radiocarbon dating"}]},{"@id":"https://cir.nii.ac.jp/crid/1360572092484228608","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Dating Lake Sediments Using Compound‐Specific <sup>14</sup>C Analysis of C<sub>16</sub> Fatty Acid: A Case Study From the Mount Fuji Volcanic Region, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360572092564001024","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Tsunamis and submarine landslides in Suruga Bay, central Japan, caused by Nankai–Suruga Trough megathrust earthquakes during the last 5000 years"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657346593792","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Volcanic and environmental influences of Mt. Fuji on the δ13C of terrestrially-derived n-alkanoic acids in sediment from Lake Yamanaka, central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418518711821056","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Paleotsunami research along the Nankai Trough and Ryukyu Trench subduction zones – Current achievements and future challenges"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1017/s0033822200057908"},{"@type":"OPENAIRE","@value":"doi_dedup___::a24c981459b30c852ab404821d9ff7f5"},{"@type":"CROSSREF","@value":"10.1016/j.earscirev.2020.103333_references_DOI_a3HkcVBgByEZflk2Cc5z5TT7sRR"},{"@type":"CROSSREF","@value":"10.1186/s40645-016-0092-7_references_DOI_a3HkcVBgByEZflk2Cc5z5TT7sRR"},{"@type":"CROSSREF","@value":"10.1016/j.orggeochem.2018.02.002_references_DOI_a3HkcVBgByEZflk2Cc5z5TT7sRR"},{"@type":"CROSSREF","@value":"10.1029/2020gc009544_references_DOI_a3HkcVBgByEZflk2Cc5z5TT7sRR"},{"@type":"CROSSREF","@value":"10.1016/j.quascirev.2020.106527_references_DOI_a3HkcVBgByEZflk2Cc5z5TT7sRR"},{"@type":"CROSSREF","@value":"10.1016/j.qsa.2024.100207_references_DOI_a3HkcVBgByEZflk2Cc5z5TT7sRR"},{"@type":"CROSSREF","@value":"10.1016/j.quascirev.2018.09.001_references_DOI_a3HkcVBgByEZflk2Cc5z5TT7sRR"},{"@type":"CROSSREF","@value":"10.1016/j.quascirev.2017.12.013_references_DOI_a3HkcVBgByEZflk2Cc5z5TT7sRR"}]}