{"@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/1363670319725918720.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1038/366234a0"}},{"identifier":{"@type":"URI","@value":"http://www.nature.com/articles/366234a0"}},{"identifier":{"@type":"URI","@value":"http://www.nature.com/articles/366234a0.pdf"}},{"identifier":{"@type":"NAID","@value":"30013848727"}}],"dc:title":[{"@value":"Geomagnetic field intensity and reversals during the past four million years"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383670319725918720","@type":"Researcher","foaf:name":[{"@value":"Jean-pierre Valet"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670319725918721","@type":"Researcher","foaf:name":[{"@value":"Laure Meynadier"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00280836"},{"@type":"EISSN","@value":"14764687"}],"prism:publicationName":[{"@value":"Nature"}],"dc:publisher":[{"@value":"Springer Science and Business Media LLC"}],"prism:publicationDate":"1993-11","prism:volume":"366","prism:number":"6452","prism:startingPage":"234","prism:endingPage":"238"},"reviewed":"false","dc:rights":["http://www.springer.com/tdm"],"url":[{"@id":"http://www.nature.com/articles/366234a0"},{"@id":"http://www.nature.com/articles/366234a0.pdf"}],"createdAt":"2003-06-12","modifiedAt":"2023-05-17","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360004229800814336","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Low‐temperature magnetic properties of pelagic carbonates: Oxidation of biogenic magnetite and identification of magnetosome chains"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004233289796480","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A detailed paleomagnetic record between 2.1 and 2.75 Ma at IODP Site U1314 in the North Atlantic: Geomagnetic excursions and the Gauss‐Matuyama transition"}]},{"@id":"https://cir.nii.ac.jp/crid/1360005518171904768","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Relative Paleointensity and Inclination Anomaly Over the Last 8 Myr Obtained From the Integrated Ocean Drilling Program Site U1335 Sediments in the Eastern Equatorial Pacific"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182088728704","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A middle Miocene relative paleointensity record from the Equatorial Pacific"}]},{"@id":"https://cir.nii.ac.jp/crid/1360588379378518784","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Miocene Magnetostratigraphy and Relative Paleointensity of Deep‐Sea Sediments at IODP Site U1490 in the Western Equatorial Pacific"}]},{"@id":"https://cir.nii.ac.jp/crid/1360588379383159168","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Linearity of natural versus laboratory-imparted remanence demagnetization diagram and reliability of relative paleointensity estimation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360588380162836224","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Reconstruction of high-resolution paleomagnetic variations in the middle Gauss chronozone, including the upper and lower boundaries of the Mammoth reversed subchronozone"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846640846305664","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Post-depositional remanent magnetization lock-in for marine sediments deduced from 10Be and paleomagnetic records through the Matuyama–Brunhes boundary"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848660683910400","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Reliability of Relative Paleointensity Recorded in Chinese Loess–Paleosol Sediments"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205318312832","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Near-bottom Magnetic Measurements with Submersible Shinkai 6500"},{"@value":"しんかいで地磁気を測る"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206238093824","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Relative geomagnetic intensity as a tool for high resolution stratigraphy"},{"@language":"ja","@value":"高精度年代対比ツールとしての古地磁気強度層序"},{"@language":"ja-Kana","@value":"コウセイド ネンダイ タイヒ ツール ト シテ ノ コ チジキ キョウドソウ ジョ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206496109568","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Recent Progress in Paleomagnetic and Rock-magnetic Studies of the Quaternary in Japan."}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206510004096","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Magnetic intensity loss and core diagenesis in long-core samples from the East Cortez Basin and the San Nicolas Basin (California Borderland)"},{"@value":"Magnetic intencity loss and core diagenesis in long-core samples from the East Cortez and the San Nicolas Basin(California Borderland)"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206514023424","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Geomagnetic paleointensity over 1.2 Ma from deep-tow vector magnetic data across the East Pacific Rise"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679206471680","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Marine Magnetic Anomalies Connected to Paleomagnetic Intensity Variation"},{"@value":"海洋地磁気異常は何を映すか？―地磁気異常と古地磁気強度変化の関連―"},{"@language":"ja-Kana","@value":"カイヨウ チジキ イジョウ ワ ナニ オ ウツス カ チジキ イジョウ ト コ チジキ キョウド ヘンカ ノ カンレン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679281362944","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"八ヶ岳火山列の古地磁気"},{"@language":"en","@value":"Paleomagnetic Properties of the Yatsugatake Volcanic Chain, Central Japan"},{"@language":"ja-Kana","@value":"ヤツガタケ カザンレツ ノ コ チジキ"}]},{"@id":"https://cir.nii.ac.jp/crid/2050870367122058240","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"UDECON : deconvolution optimization software for restoring high-resolution records from pass-through paleomagnetic measurements"}]},{"@id":"https://cir.nii.ac.jp/crid/2051151841909874560","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Toward robust deconvolution of pass-through paleomagnetic measurements : new tool to estimate magnetometer sensor response and laser interferometry of sample positioning accuracy"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1038/366234a0"},{"@type":"CIA","@value":"30013848727"},{"@type":"CROSSREF","@value":"10.1002/2013jb010381_references_DOI_J8Bu0n1dgmTuMuJqRKXudM4b8CD"},{"@type":"CROSSREF","@value":"10.1029/2012gc004080_references_DOI_J8Bu0n1dgmTuMuJqRKXudM4b8CD"},{"@type":"CROSSREF","@value":"10.1186/s40623-016-0493-2_references_DOI_J8Bu0n1dgmTuMuJqRKXudM4b8CD"},{"@type":"CROSSREF","@value":"10.1029/2018jb016209_references_DOI_J8Bu0n1dgmTuMuJqRKXudM4b8CD"},{"@type":"CROSSREF","@value":"10.1186/bf03351835_references_DOI_J8Bu0n1dgmTuMuJqRKXudM4b8CD"},{"@type":"CROSSREF","@value":"10.1186/bf03352237_references_DOI_J8Bu0n1dgmTuMuJqRKXudM4b8CD"},{"@type":"CROSSREF","@value":"10.1186/s40623-015-0332-x_references_DOI_J8Bu0n1dgmTuMuJqRKXudM4b8CD"},{"@type":"CROSSREF","@value":"10.5575/geosoc.117.1_references_DOI_J8Bu0n1dgmTuMuJqRKXudM4b8CD"},{"@type":"CROSSREF","@value":"10.1029/2024jb029694_references_DOI_J8Bu0n1dgmTuMuJqRKXudM4b8CD"},{"@type":"CROSSREF","@value":"10.1186/s40623-025-02140-w_references_DOI_J8Bu0n1dgmTuMuJqRKXudM4b8CD"},{"@type":"CROSSREF","@value":"10.1186/s40623-024-02114-4_references_DOI_J8Bu0n1dgmTuMuJqRKXudM4b8CD"},{"@type":"CROSSREF","@value":"10.1111/j.1755-6724.2012.00747.x_references_DOI_J8Bu0n1dgmTuMuJqRKXudM4b8CD"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2011.08.038_references_DOI_J8Bu0n1dgmTuMuJqRKXudM4b8CD"},{"@type":"CROSSREF","@value":"10.5918/jamstecr.2009.111_references_DOI_J8Bu0n1dgmTuMuJqRKXudM4b8CD"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2013.04.038_references_DOI_J8Bu0n1dgmTuMuJqRKXudM4b8CD"}]}