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
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- Material Type
- 記事
- Author/Editor
- Takumi KonishiMakoto Okada
- Publication, Distribution, etc.
- Publication Date
- 2020-08-08
- Publication Date (W3CDTF)
- 2020-08-08
- Periodical title
- Progress in earth and planetary science
- No. or year of volume/issue
- 7(35)
- Volume
- 7(35)
- ISSN (Periodical Title)
- 2197-4284
- ISSN-L (Periodical Title)
- 2197-4284
- Text Language Code
- eng
- DOI
- 10.1186/s40645-020-00352-0
- Persistent ID (NDL)
- info:ndljp/pid/11616277
- Collection
- Collection (Materials For Handicapped People:1)
- Collection (particular)
- 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
- Acquisition Basis
- オンライン資料収集制度
- Date Accepted (W3CDTF)
- 2021-01-13T14:13:05+09:00
- Date Captured (W3CDTF)
- 2021-01-13
- Format (IMT)
- application/pdf
- Access Restrictions
- 国立国会図書館内限定公開
- Service for the Digitized Contents Transmission Service
- 図書館・個人送信対象外
- Availability of remote photoduplication service
- 可
- Periodical Title (URI)
- Periodical Title (Persistent ID (NDL))
- info:ndljp/pid/11467724
- Data Provider (Database)
- 国立国会図書館 : 国立国会図書館デジタルコレクション
- Summary, etc.
- 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
- DOI
- 10.1186/s40645-020-00352-0
- Access Restrictions
- インターネット公開
- Related Material (URI)
- Is Referenced By
- A record of the lower Mammoth geomagnetic polarity reversal from a marine succession in the Boso Peninsula, central JapanReconstruction of high-resolution paleomagnetic variations in the middle Gauss chronozone, including the upper and lower boundaries of the Mammoth reversed subchronozone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”
- References
- Millennial-scale hydrographic changes in the northwestern Pacific during marine isotope stage 19: teleconnection with ice melt in the North AtlanticPaleoclimatic and paleoceanographic records of Marine Isotope Stage 19 at the Chiba composite section, central Japan: a reference for the Early-Middle Pleisotocene boundaryMagnetic properties of sedimentary greigite (Fe<sub>3</sub>S<sub>4</sub>): An updateCosmogenic signature of geomagnetic reversals and excursions from the Réunion event to the Matuyama–Brunhes transition (0.7–2.14 Ma interval)Relative paleointensity record during the last 800 ka from the equatorial Indian Ocean: Implication for relationship between inclination and intensity variationsNondipole FieldCalcareous nannofossil biochronology from the upper Pliocene to lower Pleistocene in the southernmost Boso Peninsula, central part of the Pacific side of JapanSedimentary records of relative paleointensity of the geomagnetic field: Theory and practiceHallmarks of maghemitization in low‐temperature remanence cycling of partially oxidized magnetite nanoparticlesEvidence from lava flows for complex polarity transitions: the new composite Steens Mountain reversal recordPolarity Reversals from Paleomagnetic Observations and Numerical Dynamo SimulationsHigh-resolution 10Be and paleomagnetic recording of the last polarity reversal in the Chiba composite section: Age and dynamics of the Matuyama–Brunhes transitionTheory 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 dataThe Matuyama-Brunhes boundary interval (500-900 ka) in North Atlantic drift sedimentsBehaviour of the geomagnetic field during the Matuyama–Brunhes polarity transitionPost-depositional remanent magnetization lock-in for marine sediments deduced from 10Be and paleomagnetic records through the Matuyama–Brunhes boundaryAge of Matuyama-Brunhes boundary constrained by U-Pb zircon dating of a widespread tephraSedimentary processes and depositional environments of a continuous marine succession across the Lower–Middle Pleistocene boundary: Kokumoto Formation, Kazusa Group, central JapanCautionary note on magnetic grain‐size estimation using the ratio of ARM to magnetic susceptibilityA geomagnetic paleointensity stack between 0.8 and 3.0 Ma from equatorial Pacific sediment coresGeomagnetic dipole strength and reversal rate over the past two million yearsThe effect of oxidation on the Verwey transition in magnetiteThe least-squares line and plane and the analysis of palaeomagnetic dataStability of mantle control over dynamo flux since the mid-CenozoicResolving the Origin of Pseudo‐Single Domain Magnetic BehaviorDipolar reversal states of the geomagnetic field and core–mantle dynamicsGeomagnetic excursions and paleointensities in the Matuyama Chron at Ocean Drilling Program Sites 983 and 984 (Iceland Basin)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 SubchronTiming of Quaternary geomagnetic reversals and excursions in volcanic and sedimentary archivesDynamical similarity of geomagnetic field reversalsTime variations in geomagnetic intensityA Critical Appraisal of the “Day” DiagramStacking paleointensity and oxygen isotope data for the last 1.5 Myr (PISO-1500)Inferred time- and temperature-dependent cation ordering in natural titanomagnetitesWhen and why sediments fail to record the geomagnetic field during polarity reversalsElectronic Conduction of Magnetite (Fe3O4) and its Transition Point at Low TemperaturesWhy are geomagnetic excursions not always recorded in sediments? Constraints from post-depositional remanent magnetization lock-in modellingDeciphering records of geomagnetic reversalsComplexity in Matuyama–Brunhes polarity transitions from North Atlantic IODP/ODP deep-sea sitesGeomagnetic, cosmogenic and climatic changes across the last geomagnetic reversal from Equatorial Indian Ocean sedimentsStratigraphy of the Kazusa Group, Boso Peninsula: An expanded and highly-resolved marine sedimentary record from the Lower and Middle Pleistocene of central JapanLong-lived transitional states of the geomagnetic field and the two dynamo families房総半島南端地域に分布する千倉・豊房層群（鮮新‐更新統）の古地磁気および微化石層序房総半島南端地域の海成上部新世界房總南端 : 新第三紀層房総半島における古地磁気層位学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Additional file 1: of A record of the upper Olduvai geomagnetic polarity transition from a sediment core in southern Yokohama City, Pacific side of central JapanPaleointensity of ODP Site 162-984Declination and inclination of ODP Site 162-984A record of the upper Olduvai geomagnetic polarity transition from a sediment core in southern Yokohama City, Pacific side of central JapanPliocene integrated chronostratigraphy from the Anno Formation, Awa Group, Boso Peninsula, central Japan, and its paleoceanographic implicationsPaleomagnetic 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
- References (URI)
- Data Provider (Database)
- 国立情報学研究所 : CiNii Research
- Original Data Provider (Database)
- 雑誌記事索引データベースCrossref科学研究費助成事業データベースCrossrefCrossrefCrossrefCrossref
- Bibliographic ID (NDL)
- 11616277