{"@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/2051996266844300032.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"NDL_BIB_ID","@value":"10319696"}},{"identifier":{"@type":"DOI","@value":"10.1186/s40623-017-0627-1"}},{"identifier":{"@type":"URI","@value":"http://id.ndl.go.jp/digimeta/10319696"}},{"identifier":{"@type":"URI","@value":"https://dl.ndl.go.jp/pid/10319696"}},{"identifier":{"@type":"URI","@value":"http://link.springer.com/content/pdf/10.1186/s40623-017-0627-1.pdf"}},{"identifier":{"@type":"URI","@value":"http://link.springer.com/article/10.1186/s40623-017-0627-1/fulltext.html"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Paleomagnetic direction and paleointensity variations during the Matuyama-Brunhes polarity transition from a marine succession in the Chiba composite section of the Boso Peninsula, central Japan"}],"dcterms:alternative":[{"@value":"Paleomagnetic direction and paleointensity variations during the Matuyama-Brunhes polarity transition from a marine succession in the Chiba composite section of the Boso Peninsula, central Japan"}],"dc:language":"en","description":[{"notation":[{"@value":"収集根拠 : オンライン資料収集制度"},{"@value":"資料形態 : テキストデータ"},{"@value":"コレクション : 国立国会図書館デジタルコレクション > 電子書籍・電子雑誌 > その他"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1420282801181482752","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"00250978"},{"@type":"NRID","@value":"1000000250978"},{"@type":"KAKEN_RESEARCHERS","@value":"12101401"},{"@type":"NRID","@value":"1000012101401"},{"@type":"ORCID","@value":"0000-0001-5856-1925"},{"@type":"NRID","@value":"9000409996649"},{"@type":"NRID","@value":"9000403407513"},{"@type":"NRID","@value":"9000347192113"},{"@type":"NRID","@value":"9000412664988"},{"@type":"NRID","@value":"9000001086810"},{"@type":"NRID","@value":"9000254740219"},{"@type":"NRID","@value":"9000386337845"},{"@type":"NRID","@value":"9000368412355"},{"@type":"NRID","@value":"9000411657404"},{"@type":"NRID","@value":"9000258415945"},{"@type":"NRID","@value":"9000267794828"},{"@type":"NRID","@value":"9000414499676"},{"@type":"NRID","@value":"9000347191132"},{"@type":"NRID","@value":"9000242676536"},{"@type":"NRID","@value":"9000391749726"},{"@type":"NRID","@value":"9000016892855"},{"@type":"NRID","@value":"9000313613726"},{"@type":"NRID","@value":"9000402935112"},{"@type":"NRID","@value":"9000000042276"},{"@type":"NRID","@value":"9000253258115"},{"@type":"NRID","@value":"9000000650055"},{"@type":"NRID","@value":"9000403551048"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/read0180444"}],"foaf:name":[{"@value":"Makoto Okada"}]},{"@id":"https://cir.nii.ac.jp/crid/1030848250430735489","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000414499653"}],"foaf:name":[{"@value":"Yuki Haneda"}]},{"@id":"https://cir.nii.ac.jp/crid/1420564276166264320","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"70431898"},{"@type":"NRID","@value":"1000070431898"},{"@type":"ORCID","@value":"0000-0003-3516-1317"},{"@type":"CINII_AUTHOR_ID","@value":"DA19482563"},{"@type":"URI","@value":"https://ci.nii.ac.jp/author/DA19482563#entity"},{"@type":"URI","@value":"https://viaf.org/viaf/NII%7CDA19482563"},{"@type":"NRID","@value":"9000004625874"},{"@type":"NRID","@value":"9000291277347"},{"@type":"NRID","@value":"9000326270630"},{"@type":"NRID","@value":"9000001427415"},{"@type":"NRID","@value":"9000414499652"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/yusuke.suganuma"}],"foaf:name":[{"@value":"Yusuke Suganuma"}]}],"publication":{"publicationIdentifier":[{"@type":"ISSN","@value":"18805981"},{"@type":"LISSN","@value":"13438832"},{"@type":"EISSN","@value":"18805981"}],"prism:publicationName":[{"@value":"EPS : Earth, Planets and Space"}],"dc:publisher":[{"@value":"Springer Nature"}],"prism:publicationDate":"2017-03-21","prism:volume":"69(45)","prism:startingPage":"45"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","url":[{"@id":"http://id.ndl.go.jp/digimeta/10319696"},{"@id":"https://dl.ndl.go.jp/pid/10319696"},{"@id":"http://link.springer.com/content/pdf/10.1186/s40623-017-0627-1.pdf"},{"@id":"http://link.springer.com/article/10.1186/s40623-017-0627-1/fulltext.html"}],"foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=Paleomagnetism","dc:title":"Paleomagnetism"},{"@id":"https://cir.nii.ac.jp/all?q=Magnetostratigraphy","dc:title":"Magnetostratigraphy"},{"@id":"https://cir.nii.ac.jp/all?q=Paleointensity","dc:title":"Paleointensity"},{"@id":"https://cir.nii.ac.jp/all?q=Marine%20isotope%20stage%20(MIS)%2019","dc:title":"Marine isotope stage (MIS) 19"},{"@id":"https://cir.nii.ac.jp/all?q=Matuyama-Brunhes%20boundary","dc:title":"Matuyama-Brunhes boundary"},{"@id":"https://cir.nii.ac.jp/all?q=Chiba%20composite%20section","dc:title":"Chiba composite section"}],"project":[{"@id":"https://cir.nii.ac.jp/crid/1040000781857443456","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"15K13581"},{"@type":"JGN","@value":"JP15K13581"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-15K13581/"}],"notation":[{"@language":"ja","@value":"海底堆積物の高解像度宇宙線生成核種分析に基づく超新星爆発イベントの探索"},{"@language":"en","@value":"Search for evidence of supernova events based on cosmogenic nuclides analysis of the marine sediment"}]},{"@id":"https://cir.nii.ac.jp/crid/1040000781899088640","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"16H04068"},{"@type":"JGN","@value":"JP16H04068"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-16H04068/"}],"notation":[{"@language":"ja","@value":"松山－ブルン地磁気逆転境界年代の決定と地質年代の総合的キャリブレーション"},{"@language":"en","@value":"Age determination for the Matuyama-Brunhes geomagnetic reversal boundary and comprehensive calibration of geologic ages"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050002213761277952","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Millennial-scale hydrographic changes in the northwestern Pacific during marine isotope stage 19: teleconnections with ice melt in the North Atlantic"},{"@value":"Millennial-scale hydrographic changes in the northwestern Pacific during marine isotope stage 19: teleconnection with ice melt in the North Atlantic"}]},{"@id":"https://cir.nii.ac.jp/crid/1050012570391873408","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A centennial-resolution terrestrial climatostratigraphy and Matuyama–Brunhes transition record from a loess sequence in China"}]},{"@id":"https://cir.nii.ac.jp/crid/1050564287496675840","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Relative paleointensity stack during the last 250 kyr in the northwest Pacific"}]},{"@id":"https://cir.nii.ac.jp/crid/1050570232449668096","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A full sequence of the Matuyama–Brunhes geomagnetic reversal in the Chiba composite section, Central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360009142452858880","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Biomarkers in the rock outcrop of the Kazusa Group reveal palaeoenvironments of the Kuroshio region"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011142931979392","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A Pliocene‐Pleistocene stack of 57 globally distributed benthic δ<sup>18</sup>O records"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011144278101632","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Cosmogenic nuclides during Isotope Stages 2 and 3"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011144514848128","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Relative paleointensity record during the last 800 ka from the equatorial Indian Ocean: Implication for relationship between inclination and intensity variations"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011144695853952","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Reconciling astrochronological and <sup>40</sup>Ar/<sup>39</sup>Ar ages for the Matuyama‐Brunhes boundary and late Matuyama Chron"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011145200120704","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"10Be evidence for the Matuyama–Brunhes geomagnetic reversal in the EPICA Dome C ice core"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011145317403008","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Linking the 8.2 ka event and its freshwater forcing in the Labrador Sea"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011145415534592","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Potbellies, wasp‐waists, and superparamagnetism in magnetic hysteresis"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011145700539776","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Response to the comment by W.H. Schwarz et al. on “Joint determination of 40K decay constants and 40Ar∗/40K for the Fish Canyon sanidine standard, and improved accuracy for 40Ar/39Ar geochronology” by P.R. Renne et al. (2010)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011146492307328","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Synchronizing Rock Clocks of Earth History"}]},{"@id":"https://cir.nii.ac.jp/crid/1360021390757712000","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Magnetostratigraphic dating of Early <scp>Miocene</scp> deep‐sea fossils from the <scp>Morozaki Group</scp> in central <scp>Japan</scp>"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292617915640576","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Evolution of Ocean Temperature and Ice Volume Through the Mid-Pleistocene Climate Transition"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292619103443712","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"First‐order reversal curve diagrams: A new tool for characterizing the magnetic properties of natural samples"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292619224311552","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Structural and temporal requirements for geomagnetic field reversal deduced from lava flows"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292619828609024","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Sedimentary records of relative paleointensity of the geomagnetic field: Theory and practice"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292621112468992","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A relative paleointensity record of the geomagnetic field since 1.6 Ma from the North Pacific"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292621606982016","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A precursor to the Matuyama/Brunhes transition-field instability as recorded in pelagic sediments"}]},{"@id":"https://cir.nii.ac.jp/crid/1360568466794951168","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"High-resolution 10Be and paleomagnetic recording of the last polarity reversal in the Chiba composite section: Age and dynamics of the Matuyama–Brunhes transition"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574092891194496","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Theory and application of the Day plot (<i>M</i><sub><i>rs</i></sub>/<i>M</i><sub><i>s</i></sub> versus <i>H</i><sub><i>cr</i></sub>/<i>H</i><sub><i>c</i></sub>) 1. Theoretical curves and tests using titanomagnetite data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574092892730112","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Hysteresis properties of titanomagnetites: Grain-size and compositional dependence"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574095361596800","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Characterizing interactions in fine magnetic particle systems using first order reversal curves"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574095618882304","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Global changes in intensity of the Earth's magnetic field during the past 800 kyr"}]},{"@id":"https://cir.nii.ac.jp/crid/1360576118729300608","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A record of the lower Mammoth geomagnetic polarity reversal from a marine succession in the Boso Peninsula, central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360579929469491712","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Rotated Transtensional Basins Formed During Back‐Arc Spreading in Japan: Simultaneous Rapid Tectonic Rotation and Basin Subsidence"}]},{"@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/1360846640846268288","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"10Be evidence for delayed acquisition of remanent magnetization in marine sediments: Implication for a new age for the Matuyama–Brunhes boundary"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846640846305664","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"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/1360846643404971392","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Age of Matuyama-Brunhes boundary constrained by U-Pb zircon dating of a widespread tephra"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657398972544","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"High resolution stratigraphy across the early–middle Pleistocene boundary from a core of the Kokumoto Formation at Tabuchi, Chiba Prefecture, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360849941664850432","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Age of the N7/N8 (M4/M5) planktonic foraminifera zone boundary: constraints from the zircon geochronology and magnetostratigraphy of early Miocene sediments in Ichishi, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855569872688512","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Beryllium-10 in deep-sea sediments: a tracer for the Earth's magnetic field intensity during the last 200,000 years"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855570474838144","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A Southern Hemisphere record of the Matuyama‐Brunhes polarity reversal"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855570746107776","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Sedimentary processes and depositional environments of a continuous marine succession across the Lower–Middle Pleistocene boundary: Kokumoto Formation, Kazusa Group, central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360857593774240000","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Depositional process of the <scp>Byk‐E</scp> tephra bed in the Chiba section, central Japan: A marker bed defining the Global Boundary Stratotype Section and Point for the Chibanian Stage"}]},{"@id":"https://cir.nii.ac.jp/crid/1361131420852922880","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Synchronizing volcanic, sedimentary, and ice core records of Earth’s last magnetic polarity reversal"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137043572822784","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Geomagnetic paleointensity and environmental record from Labrador Sea core MD95-2024: global marine sediment and ice core chronostratigraphy for the last 110 kyr"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137043579969920","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Glacio-eustatic control on deep-marine clastic forearc sedimentation, Pliocene-mid-Pleistocene (c. 1180–600 ka) Kazusa Group, SE Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137043899061120","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Rock magnetism of Late Neogene and Pleistocene deep‐sea sediments: Relationship to sediment source, diagenetic processes, and sediment lithology"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137044027316224","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Detailed paleomagnetic records during the Brunhes-Matuyama geomagnetic reversal, and a direct determination of depth lag for magnetization in marine sediments"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137044539906048","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"An ice core perspective on the age of the Matuyama–Brunhes boundary"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137044634957312","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The paleomagnetic record at IODP Site U1307 back to 2.2 Ma (Eirik Drift, off south Greenland)"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137044736297600","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Matuyama–Brunhes reversal and Kamikatsura event on Maui: paleomagnetic directions, 40 Ar/ 39 Ar ages and implications"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137045572936192","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A geomagnetic paleointensity stack between 0.8 and 3.0 Ma from equatorial Pacific sediment cores"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418518814361344","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Geomagnetic dipole strength and reversal rate over the past two million years"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418519483433472","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Age calibrated relative paleointensity for the last 1.5 Myr at IODP Site U1308 (North Atlantic)"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699993388425856","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Wasp‐waisted hysteresis loops: Mineral magnetic characteristics and discrimination of components in mixed magnetic systems"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699994971672576","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Highly resolved Beryllium-10 record from ODP Site 1089—A global signal?"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699996265963136","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"South Asian monsoon variability during the past 800kyr revealed by rock magnetic proxies"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981468867153024","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Seismotectonics at the Trench-Trench-Trench Triple Junction off Central Honshu"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981468877008896","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"An alternative astronomical calibration of the lower Pleistocene timescale based on ODP Site 677"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981470441989760","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The least-squares line and plane and the analysis of palaeomagnetic data"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262945318809856","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Paleomagnetic Evidence for Pleistocene Clockwise Rotation in the Oiso Hills: A Possible Record of Interaction Between the Philippine Sea Plate and Northeast Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262945420040320","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Relative geomagnetic paleointensity of the Brunhes Chron and the Matuyama–Brunhes precursor as recorded in sediment core from Wilkes Land Basin (Antarctica)"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544418933507200","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Relative paleointensity (RPI) and oxygen isotope stratigraphy at IODP Site U1308: North Atlantic RPI stack for 1.2–2.2 Ma (NARPI-2200) and age of the Olduvai Subchron"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544419397071232","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Relative paleointensity of the geomagnetic field during Brunhes Chron recorded in North Pacific deep-sea sediment cores: orbital influence?"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544420919384192","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Orbital modulation of the Earth's magnetic field intensity"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544421155486976","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Identification of ferromagnetic minerals in a rock by coercivity and unblocking temperature properties"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544421308551552","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Dynamical similarity of geomagnetic field reversals"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825893826864256","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Neogene–Quaternary sedimentary successions"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825893853241856","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Time variations in geomagnetic intensity"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825895689035776","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Geomagnetic palaeointensities and astrochronological ages for the Matuyama–Brunhes boundary and the boundaries of the Jaramillo Subchron: palaeomagnetic and oxygen isotope records from ODP Site 983"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825896348346368","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"North Atlantic palaeointensity stack since 75ka (NAPIS–75) and the duration of the Laschamp event"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107368275946880","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Stacking paleointensity and oxygen isotope data for the last 1.5 Myr (PISO-1500)"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107369216099968","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"An optimized multi-proxy, multi-site Antarctic ice and gas orbital chronology (AICC2012): 120–800 ka"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107369546054272","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"First‐Order Reversal Curve (FORC) Diagrams"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107370093474304","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Geomagnetic relative paleointensity chronostratigraphy of sediment cores from the Okhotsk Sea"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388843409440000","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A 2.14‐Myr astronomically tuned record of relative geomagnetic paleointensity from the western Philippine Sea"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388843802308608","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Magnetic paleointensity stratigraphy and high-resolution Quaternary geochronology: successes and future challenges"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388844555572224","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Submarine fan sequences of the lower Kazusa Group, a Plio–Pleistocene forearc basin fill in the Boso Peninsula, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388844559878656","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"How fast was the Matuyama–Brunhes geomagnetic reversal? A new subcentennial record from the Sulmona Basin, central Italy"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388844663767936","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Age through tandem correlation of Quaternary relative paleointensity (RPI) and oxygen isotope data at IODP Site U1306 (Eirik Drift, SW Greenland)"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670320058767232","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Deciphering records of geomagnetic reversals"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670321174248576","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Inferred glacio-eustatic control for high-frequency depositional sequences of the Plio-Pleistocene Kazusa Group, a forearc basin fill in Boso Peninsula, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951793325867136","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Geomagnetic, cosmogenic and climatic changes across the last geomagnetic reversal from Equatorial Indian Ocean sediments"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951794032661120","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"North Pacific response to millennial‐scale changes in ocean circulation over the last 60 kyr"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951794650101120","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Stratigraphy of the Kazusa Group, Boso Peninsula: An expanded and highly-resolved marine sedimentary record from the Lower and Middle Pleistocene of central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233268777720448","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Relative paleointensity and environmental magnetism since 1.2 Ma at IODP site U1305 (Eirik Drift, NW Atlantic)"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233268961423232","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Extremely rapid directional change during Matuyama-Brunhes geomagnetic polarity reversal"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206236847232","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"High-resolution chronology of the lower Pleistocene Otadai and Umegase Formations of the Kazusa Group, Boso Peninsula, central Japan -Chronostratigraphy of the JNOC TR-3 cores based on oxygen isotope, magnetostratigraphy and calcareous nannofossil-"},{"@language":"ja","@value":"房総半島に分布する下部更新統上総層群大田代層と梅ヶ瀬層の高精度堆積年代―石油公団研究井TR-3コアの酸素同位体比・古地磁気・石灰質ナンノ化石に基づく年代層序―"},{"@language":"ja-Kana","@value":"ボウソウ ハントウ ニ ブンプ スル カブ コウシントウ カズサソウグン オオタダイソウ ト ウメガセソウ ノ コウセイド タイセキ ネンダイ セキユ コウダン ケンキュウイ TR 3 コア ノ サンソ ドウイタイヒ コ チジキ セッカイシツ ナンノ カセキ ニ モトヅク ネンダイソウ ジョ"},{"@value":"High-resolution chronology of the lower Pleistocene Otadai and Umegase formations of the Kazusa group, Boso Peninsula, central JapandChronostratig- raphy of the JNOC TR-3 cores based on oxygen isotope, magnetostratigraphy and calcareous nanofossil"},{"@value":"High-resolution chronology of the lower Pleistocene Otadai and Umegase formations of the Kazusa group, Boso Peninsula, central Japan—Chronostratigraphy of the JNOC TR-3 cores based on oxygen isotope, magnetostratigraphy and calcareous nanofossil"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206241992576","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Magnetostratigraphy of the Ryukyu Group in Miyakojima Island, Okinawa, Japan"},{"@language":"ja","@value":"宮古島に分布する琉球層群の磁気層序"},{"@language":"ja-Kana","@value":"ミヤコジマ ニ ブンプ スル リュウキュウソウグン ノ ジキソウ ジョ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206497011840","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Diatom Biostratigraphy of the Kazusa Group, Boso Peninsula, Honshu, Japan."},{"@language":"ja","@value":"房総半島上総層群の珪藻生層序"},{"@value":"Marine diatoms of the Kazusa group in the type locality of the Boso Peninsula, Honsu, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390016494575405568","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"古地磁気層序とテフラ層序に基づく房総半島南部の下部更新統千倉層群と同半島東部の上総層群の対比"},{"@language":"en","@value":"Stratigraphic correlation between the lower Pleistocene Chikura Group in the southern part of the Boso Peninsula and the Kazusa Group in the eastern part of the peninsula, based on magneto- and tephro-stratigraphy"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681218901632","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"An integrated stratigraphy around the Plio-Pleistocene boundary interval in the Chikura Group, southernmost part of the Boso Peninsula, central Japan, based on data from paleomagnetic and oxygen isotopic analyses"},{"@language":"ja","@value":"房総半島南端千倉層群における鮮新統－更新統境界層準の古地磁気－酸素同位体複合層序"},{"@language":"ja-Kana","@value":"ボウソウ ハントウ ナンタン センソウソウグン ニ オケル センシントウ-コウシントウ キョウカイソウ ジュン ノ コ チジキ-サンソ ドウイタイ フクゴウソウ ジョ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681485527296","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Further application of the deconvolution method of post-depositional DRM to the precise record of the Matuyama-Brunhes reversal in the sediments from the Boso Peninsula, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282763107304576","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A summary of the Chiba Section, Japan"},{"@language":"ja","@value":"千葉セクション"},{"@value":"千葉セクション : 下部-中部更新統境界の国際境界模式層断面とポイントへの提案書(要約)"},{"@language":"ja-Kana","@value":"チバ セクション : カブ-チュウブ コウシントウ キョウカイ ノ コクサイ キョウカイモシキソウ ダンメン ト ポイント エ ノ テイアンショ(ヨウヤク)"}]},{"@id":"https://cir.nii.ac.jp/crid/1390573242828088832","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"西三河平野西南部油ヶ淵低地下の更新統古地磁気層序"},{"@language":"en","@value":"Subsurface Pleistocene magnetostratigraphy under the Aburagafuchi Lowland in the southwestern Nishi-mikawa Plain, central Japan"},{"@language":"ja-Kana","@value":"ニシミカワ ヘイヤ ニシナンブユ ヶ エン テイチカ ノ コウシントウ コ チジキソウ ジョ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390577144549462528","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Chibanian GSSP site and the stratigraphy of an on-land forearc basin Kazusa Group"},{"@language":"ja","@value":"チバニアンGSSPサイトと陸化した前弧海盆上総層群の層序"}]},{"@id":"https://cir.nii.ac.jp/crid/1880865117650024960","@type":"Dataset","relationType":["isSupplementedBy"],"jpcoar:relatedTitle":[{"@value":"MOESM2 of Paleomagnetic direction and paleointensity variations during the Matuyama–Brunhes polarity transition from a marine succession in the Chiba composite section of the Boso Peninsula, central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1881146593187611392","@type":"Dataset","relationType":["isSupplementedBy"],"jpcoar:relatedTitle":[{"@value":"MOESM1 of Paleomagnetic direction and paleointensity variations during the Matuyamaâ  Brunhes polarity transition from a marine succession in the Chiba composite section of the Boso Peninsula, central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/2050307417121633536","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A paleomagnetic record of the early Matuyama chron including the Reunion subchron and the onset Olduvai boundary : high-resolution magnetostratigraphy and insights from transitional geomagnetic fields"}]},{"@id":"https://cir.nii.ac.jp/crid/2050307417125249792","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Multiproxy sedimentological and geochemical analyses across the Lower–Middle Pleistocene boundary : chemostratigraphy and paleoenvironment of the Chiba composite section, central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/2050870367075055232","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Calcareous nannofossil biostratigraphy of the Lower–Middle Pleistocene boundary of the GSSP, Chiba composite section in the Kokumoto Formation, Kazusa Group, central Japan, and implications for sea-surface environmental changes"}]},{"@id":"https://cir.nii.ac.jp/crid/2051151842058306048","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Paleoceanography and dinoflagellate cyst stratigraphy across the Lower–Middle Pleistocene Subseries (Calabrian–Chibanian Stage) boundary at the Chiba composite section, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/2051433317037092480","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Millennial-scale oscillations in the Kuroshio–Oyashio boundary during MIS 19 based on the radiolarian record from the Chiba composite section, central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/2051714792011723008","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Paleoceanography of the northwestern Pacific across the Early–Middle Pleistocene boundary (Marine Isotope Stages 20–18)"}]},{"@id":"https://cir.nii.ac.jp/crid/2051714792015345024","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Matuyama-Brunhes geomagnetic reversal record and associated key tephra layers in Boso Peninsula : extraction of primary magnetization of geomagnetic fields from mixed magnetic minerals of depositional, diagenesis, and weathering processes"}]},{"@id":"https://cir.nii.ac.jp/crid/2051714792052187392","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A sedimentary paleomagnetic record of the upper Jaramillo transition from the Lantian Basin in China"}]},{"@id":"https://cir.nii.ac.jp/crid/2051996266990514432","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Preface for the article collection “stratigraphy and paleoclimatic/paleoenvironmental evolution across the Early–Middle Pleistocene transition in the Chiba composite section, Japan, and other reference sections in East Asia”"}]}],"dataSourceIdentifier":[{"@type":"NDL_SEARCH","@value":"oai:ndlsearch.ndl.go.jp:R100000039-I10319696"},{"@type":"CROSSREF","@value":"10.1186/s40623-017-0627-1"},{"@type":"KAKEN","@value":"PRODUCT-20848504"},{"@type":"KAKEN","@value":"PRODUCT-22467231"},{"@type":"OPENAIRE","@value":"doi_dedup___::fd3325e7ede2a9cfc311ec124d19e4a6"},{"@type":"CROSSREF","@value":"10.1038/s43247-021-00154-2_references_DOI_LdjN8WhcixFClxL6BZqLBTxVVQx"},{"@type":"CROSSREF","@value":"10.1186/s40645-020-00337-z_references_DOI_LdjN8WhcixFClxL6BZqLBTxVVQx"},{"@type":"CROSSREF","@value":"10.1186/s40645-021-00438-3_references_DOI_LdjN8WhcixFClxL6BZqLBTxVVQx"},{"@type":"CROSSREF","@value":"10.1186/s40645-022-00468-5_references_DOI_LdjN8WhcixFClxL6BZqLBTxVVQx"},{"@type":"CROSSREF","@value":"10.1111/iar.12513_references_DOI_LdjN8WhcixFClxL6BZqLBTxVVQx"},{"@type":"CROSSREF","@value":"10.1016/j.chemgeo.2019.119333_references_DOI_LdjN8WhcixFClxL6BZqLBTxVVQx"},{"@type":"CROSSREF","@value":"10.1186/s40645-020-00355-x_references_DOI_LdjN8WhcixFClxL6BZqLBTxVVQx"},{"@type":"CROSSREF","@value":"10.1186/s40623-022-01626-1_references_DOI_LdjN8WhcixFClxL6BZqLBTxVVQx"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2019.05.004_references_DOI_LdjN8WhcixFClxL6BZqLBTxVVQx"},{"@type":"CROSSREF","@value":"10.1186/s40645-020-00352-0_references_DOI_LdjN8WhcixFClxL6BZqLBTxVVQx"},{"@type":"CROSSREF","@value":"10.1186/s40645-020-00354-y_references_DOI_LdjN8WhcixFClxL6BZqLBTxVVQx"},{"@type":"CROSSREF","@value":"10.1093/gji/ggab352_references_DOI_LdjN8WhcixFClxL6BZqLBTxVVQx"},{"@type":"CROSSREF","@value":"10.1186/s40645-021-00465-0_references_DOI_LdjN8WhcixFClxL6BZqLBTxVVQx"},{"@type":"CROSSREF","@value":"10.9795/bullgsj.73.1_references_DOI_LdjN8WhcixFClxL6BZqLBTxVVQx"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2023.0014_references_DOI_LdjN8WhcixFClxL6BZqLBTxVVQx"},{"@type":"CROSSREF","@value":"10.1029/2022tc007642_references_DOI_LdjN8WhcixFClxL6BZqLBTxVVQx"},{"@type":"CROSSREF","@value":"10.1186/s40623-024-02114-4_references_DOI_LdjN8WhcixFClxL6BZqLBTxVVQx"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2017.0052_references_DOI_LdjN8WhcixFClxL6BZqLBTxVVQx"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2018.0056_references_DOI_LdjN8WhcixFClxL6BZqLBTxVVQx"},{"@type":"CROSSREF","@value":"10.1186/s40645-020-00395-3_references_DOI_LdjN8WhcixFClxL6BZqLBTxVVQx"},{"@type":"CROSSREF","@value":"10.1186/s40645-020-00393-5_references_DOI_LdjN8WhcixFClxL6BZqLBTxVVQx"},{"@type":"CROSSREF","@value":"10.1111/iar.12432_references_DOI_LdjN8WhcixFClxL6BZqLBTxVVQx"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2022.0060_references_DOI_LdjN8WhcixFClxL6BZqLBTxVVQx"},{"@type":"CROSSREF","@value":"10.1126/sciadv.aaw4621_references_DOI_LdjN8WhcixFClxL6BZqLBTxVVQx"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2019.115936_references_DOI_LdjN8WhcixFClxL6BZqLBTxVVQx"}]}