{"@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/1360011146429360640.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1186/bf03352845"}},{"identifier":{"@type":"URI","@value":"https://link.springer.com/content/pdf/10.1186/BF03352845.pdf"}},{"identifier":{"@type":"URI","@value":"https://link.springer.com/article/10.1186/BF03352845/fulltext.html"}},{"identifier":{"@type":"URI","@value":"http://link.springer.com/content/pdf/10.1186/BF03352845"}}],"dc:title":[{"@value":"Paleomagnetic directions of the Gauss-Matuyama polarity transition recorded in drift sediments (IODP Site U1314) in the North Atlantic"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title>\n          <jats:p>The geomagnetic field direction during the Gauss-Matuyama (G-M) polarity transition was investigated from a high-accumulation-rate (≥10 cm/kyr) sediment core drilled in the Gardar drift in the North Atlantic at Site U1314 during Expedition 306 of the Integrated Ocean Drilling Program (IODP). A well-defined characteristic remanent magnetization was generally obtained by alternating field demagnetization. The consistency of the results with records from Icelandic lavas confirms that the North Atlantic drift sediments contain a high-fidelity record of the geomagnetic field change. During the G-M transition, the virtual geomagnetic pole (VGP) latitude shows north-south-north-south rebounding, with the three VGP paths falling within different longitudinal bands. Two of the three paths are close to or within the preferred bands in which transitional VGPs are suggested to be longitudinally confined. Three additional loops occur that approach mid-to-low latitudes from the North or South pole regions. In addition, the VGPs show rapid movement (directional jumps) between VGP clusters.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380011146429360640","@type":"Researcher","foaf:name":[{"@value":"Masao Ohno"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011146429360645","@type":"Researcher","foaf:name":[{"@value":"Fumi Murakami"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011146429360647","@type":"Researcher","foaf:name":[{"@value":"Fumiki Komatsu"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011146429360644","@type":"Researcher","foaf:name":[{"@value":"Yohan Guyodo"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011146429360643","@type":"Researcher","foaf:name":[{"@value":"Gary Acton"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011146429360646","@type":"Researcher","foaf:name":[{"@value":"Toshiya Kanamatsu"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011146429360641","@type":"Researcher","foaf:name":[{"@value":"Helen F. Evans"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011146429360642","@type":"Researcher","foaf:name":[{"@value":"Futoshi Nanayama"}]}],"publication":{"publicationIdentifier":[{"@type":"EISSN","@value":"18805981"}],"prism:publicationName":[{"@value":"Earth, Planets and Space"}],"dc:publisher":[{"@value":"Springer Science and Business Media LLC"}],"prism:publicationDate":"2008-09","prism:volume":"60","prism:number":"9","prism:startingPage":"e13","prism:endingPage":"e16"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["https://creativecommons.org/licenses/by/4.0/","https://creativecommons.org/licenses/by/4.0/"],"url":[{"@id":"https://link.springer.com/content/pdf/10.1186/BF03352845.pdf"},{"@id":"https://link.springer.com/article/10.1186/BF03352845/fulltext.html"},{"@id":"http://link.springer.com/content/pdf/10.1186/BF03352845"}],"createdAt":"2014-08-15","modifiedAt":"2021-09-02","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360004229801733504","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Deconvolution of continuous paleomagnetic data from pass‐through magnetometer: A new algorithm to restore geomagnetic and environmental information based on realistic optimization"}]},{"@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/1390282681216690304","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Lithology and upper boundary of the Olduvai Subchronozone in a core recovered from the middle Kazusa Group (Lower Pleistocene) on the Miura Peninsula, Pacific side of central Japan"},{"@language":"ja","@value":"三浦半島北部の上総層群中部（下部更新統）で掘削されたコアの堆積相とオルドバイ正磁極亜帯の上限"},{"@language":"ja-Kana","@value":"ミウラ ハントウ ホクブ ノ カズサソウグン チュウブ(カブ コウシントウ)デ クッサク サレタ コア ノ タイセキソウ ト オルドバイ セイ ジキョク アタイ ノ ジョウゲン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681217874944","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Late Pliocene magneto- and climatostratigraphic evolution toward the onset of the Quaternary in East Asia"},{"@language":"ja","@value":"古地磁気・古気候層序からみた東アジアの第四紀の始まり"},{"@language":"ja-Kana","@value":"コ チジキ ・ コ キコウソウ ジョ カラ ミタ ヒガシアジア ノ ダイシキ ノ ハジマリ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681218478720","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Gauss-Matuyama polarity reversal horizon in the Tokai Group, central Japan, suggested from detailed rock magnetic and paleomagnetic studies"},{"@language":"ja","@value":"岩石磁気・古地磁気測定から示唆される東海層群のガウス-松山逆転層準"},{"@language":"ja-Kana","@value":"ガンセキ ジキ ・ コ チジキ ソクテイ カラ シサ サレル トウカイソウグン ノ ガウス : マツヤマ ギャクテンソウ ジュン"}]},{"@id":"https://cir.nii.ac.jp/crid/2050025942005880192","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A record of the upper Olduvai geomagnetic polarity transition from a sediment core in southern Yokohama City, Pacific side of central Japan"}]},{"@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":"10.1186/bf03352845"},{"@type":"OPENAIRE","@value":"doi_dedup___::a6aeadbb5dd4b7d5d899a97a9cf805db"},{"@type":"CROSSREF","@value":"10.1002/2014gc005513_references_DOI_N6qc8sMNnodEMzcHHtywgUfJt6y"},{"@type":"CROSSREF","@value":"10.1029/2012gc004080_references_DOI_N6qc8sMNnodEMzcHHtywgUfJt6y"},{"@type":"CROSSREF","@value":"10.1186/s40623-016-0493-2_references_DOI_N6qc8sMNnodEMzcHHtywgUfJt6y"},{"@type":"CROSSREF","@value":"10.1186/s40645-016-0104-7_references_DOI_N6qc8sMNnodEMzcHHtywgUfJt6y"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2014.0002_references_DOI_N6qc8sMNnodEMzcHHtywgUfJt6y"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2011.0008_references_DOI_N6qc8sMNnodEMzcHHtywgUfJt6y"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2014.0034_references_DOI_N6qc8sMNnodEMzcHHtywgUfJt6y"}]}