{"@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/1360011146425612928.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/s0969-8043(00)00094-4"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0969804300000944?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0969804300000944?httpAccept=text/plain"}},{"identifier":{"@type":"PMID","@value":"10836453"}},{"identifier":{"@type":"NAID","@value":"30002957518"}}],"dc:title":[{"@value":"Formation and decay of the E1′ center and of its precursor"}],"description":[{"notation":[{"@value":"The E1' center has been used for ESR dating of quartz with assuming that the signal intensity increases with natural radiation dose as those of other ESR signals do. However, this simple assumption is not necessarily correct. Formation and decay of the E1' center are closely related with its precursor, diamagnetic oxygen vacancies. Gamma ray of large dose (100 kGy) creates oxygen vacancies giving little dose rate effect, which, therefore, might be useful for dating of granites and high dose dosimetry."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380011146425612928","@type":"Researcher","foaf:name":[{"@value":"Shin Toyoda"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011146425612929","@type":"Researcher","foaf:name":[{"@value":"Wataru Hattori"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"09698043"},{"@type":"NCID","@value":"AA10874887"}],"prism:publicationName":[{"@value":"Applied Radiation and Isotopes"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2000-05","prism:volume":"52","prism:number":"5","prism:startingPage":"1351","prism:endingPage":"1356"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S0969804300000944?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S0969804300000944?httpAccept=text/plain"}],"createdAt":"2002-07-25","modifiedAt":"2019-04-14","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050306506455869440","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Millennial-scale East Asian Summer Monsoon variability recorded in grain size and provenance of mud belt sediments on the inner shelf of the East China Sea during mid-to late Holocene"},{"@value":"Millennial-scale East Asian Summer Monsoon variability recorded in grain size and province of mud belt sediments on the inner shelf of the East China Sea during mid-to late Holocene"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004230119508736","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"ESR signal intensity and crystallinity of quartz from Gobi and sandy deserts in East Asia and implication for tracing Asian dust provenance"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285712820873984","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Electron spin resonance signals of quartz in present-day river bed sediments and possible source rocks in the Kizu River basin, Western Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285713972844928","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Investigation of the temporal change of the sources of Aeolian dust delivered to East Asia using electron spin resonance signals in quartz"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565165845799168","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Contribution of detrital materials from the Yukon River to the continental shelf sediments of the Bering Sea based on the electron spin resonance signal intensity and crystallinity of quartz"}]},{"@id":"https://cir.nii.ac.jp/crid/1360572092555849472","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Origin of aeolian dust emitted from the Tarim Basin based on the ESR signal intensity and crystallinity index of quartz: the recycling system of fine detrital material within the basin"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848654730576384","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Westerly jet‐East Asian summer monsoon connection during the Holocene"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657254627072","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Millennial-scale oscillations of the westerly jet path during the last glacial period"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657398985344","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"ESR signals in quartz: Applications to provenance research – A review"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848663926264832","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Characteristics of ESR signals and TLCLs of quartz included in various source rocks and sediments in Japan: A clue to sediment provenance"}]},{"@id":"https://cir.nii.ac.jp/crid/1520290883875993856","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@value":"Eolian Dust from the Asian Deserts to the Japanese Islands since the Last Glacial Maximum: the Basis for the ESR Method"},{"@language":"ja-Kana","@value":"Eolian Dust from the Asian Deserts to the Japanese Islands since the Last Glacial Maximum the Basis for the ESR Method"},{"@language":"ja","@value":"アジア大陸の砂漠から日本列島に運ばれた最終氷期最盛期と完新世の風成塵 : 電子スピン共鳴(ESR)分析による(<特集>レスと風成塵)"},{"@language":"en","@value":"Eolian Dust from the Asian Deserts to the Japanese Islands since the Last Glacial Maximum : the Basis for the ESR Method(<Featured Article>Loess and Eolian Dust)"}]},{"@id":"https://cir.nii.ac.jp/crid/2050588891962967808","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"ESR signal intensity of quartz in the fine-silt fraction of riverbed sediments from the Yangtze River : a provenance tracer for suspended particulate matter"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1016/s0969-8043(00)00094-4"},{"@type":"CIA","@value":"30002957518"},{"@type":"OPENAIRE","@value":"doi_dedup___::e122849ccfd69de1dfbd2169a5f32608"},{"@type":"CROSSREF","@value":"10.1002/ggge.20162_references_DOI_DdVqc48gOPBwum2ZVjohEK1t9Sx"},{"@type":"CROSSREF","@value":"10.1016/j.quaint.2015.05.048_references_DOI_DdVqc48gOPBwum2ZVjohEK1t9Sx"},{"@type":"CROSSREF","@value":"10.1186/s40645-017-0118-9_references_DOI_DdVqc48gOPBwum2ZVjohEK1t9Sx"},{"@type":"CROSSREF","@value":"10.1515/geochr-2015-0039_references_DOI_DdVqc48gOPBwum2ZVjohEK1t9Sx"},{"@type":"CROSSREF","@value":"10.2478/s13386-013-0121-x_references_DOI_DdVqc48gOPBwum2ZVjohEK1t9Sx"},{"@type":"CROSSREF","@value":"10.1016/j.dsr2.2011.12.001_references_DOI_DdVqc48gOPBwum2ZVjohEK1t9Sx"},{"@type":"CROSSREF","@value":"10.1016/j.quaint.2014.09.014_references_DOI_DdVqc48gOPBwum2ZVjohEK1t9Sx"},{"@type":"CROSSREF","@value":"10.1017/s0016756820000242_references_DOI_DdVqc48gOPBwum2ZVjohEK1t9Sx"},{"@type":"CROSSREF","@value":"10.1002/2013gc004931_references_DOI_DdVqc48gOPBwum2ZVjohEK1t9Sx"},{"@type":"CROSSREF","@value":"10.2478/s13386-013-0111-z_references_DOI_DdVqc48gOPBwum2ZVjohEK1t9Sx"},{"@type":"CROSSREF","@value":"10.1016/j.jseaes.2010.08.010_references_DOI_DdVqc48gOPBwum2ZVjohEK1t9Sx"}]}