A new mechanical perspective on a shallow megathrust near-trench slip from the high-resolution fault model of the 2011 Tohoku-Oki earthquake
国立国会図書館館内限定公開
収録元データベースで確認する
国立国会図書館デジタルコレクション
デジタルデータあり
公開元のウェブサイトで確認する
DOI[10.1186/s40645-022-00524-0]のデータに遷移します
全国の図書館の所蔵
国立国会図書館以外の全国の図書館の所蔵状況を表示します。
所蔵のある図書館から取寄せることが可能かなど、資料の利用方法は、ご自身が利用されるお近くの図書館へご相談ください
書誌情報
この資料の詳細や典拠（同じ主題の資料を指すキーワード、著者名）等を確認できます。
- 資料種別
- 記事
- 著者・編者
- Tatsuya KubotaTatsuhiko SaitoRyota Hino
- 出版年月日等
- 2022-12-05
- 出版年（W3CDTF）
- 2022-12-05
- タイトル（掲載誌）
- Progress in earth and planetary science
- 巻号年月日等（掲載誌）
- 9(68)
- 掲載巻
- 9(68)
- ISSN（掲載誌）
- 2197-4284
- ISSN-L（掲載誌）
- 2197-4284
- 本文の言語コード
- eng
- DOI
- 10.1186/s40645-022-00524-0
- 国立国会図書館永続的識別子
- info:ndljp/pid/12998709
- コレクション（共通）
- コレクション（障害者向け資料：レベル1）
- コレクション（個別）
- 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
- 収集根拠
- オンライン資料収集制度
- 受理日（W3CDTF）
- 2023-09-27T14:40:47+09:00
- 保存日（W3CDTF）
- 2023-04-11
- 記録形式（IMT）
- application/pdf
- オンライン閲覧公開範囲
- 国立国会図書館内限定公開
- デジタル化資料送信
- 図書館・個人送信対象外
- 遠隔複写可否（NDL）
- 可
- 掲載誌（国立国会図書館永続的識別子）
- info:ndljp/pid/12307811
- 連携機関・データベース
- 国立国会図書館 : 国立国会図書館デジタルコレクション
- 要約等
- 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/s40645-022-00524-010.21203/rs.3.rs-1714847/v1
- オンライン閲覧公開範囲
- インターネット公開
- 関連情報（URI）
- 参照
- Joint inversion of ocean-bottom pressure and GNSS data from the 2003 Tokachi-oki earthquakeOn the use of tsunami-source data for high-resolution fault imaging of offshore earthquakesMechanically Coupled Areas on the Plate Interface in the Kanto Region, Central Japan, Generating Great Earthquakes and Slow-Slip EventsAnisotropic structure at shallow depths across the Japan Trenchベイズ推定によるすべりインバージョン研究の高度化
- 参照
- Fault lubrication during earthquakesSeafloor observations indicate spatial separation of coseismic and postseismic slips in the 2011 Tohoku earthquakeLow Coseismic Shear Stress on the Tohoku-Oki Megathrust Determined from Laboratory ExperimentsStructure and Composition of the Plate-Boundary Slip Zone for the 2011 Tohoku-Oki EarthquakeCoseismic slip model of offshore moderate interplate earthquakes on March 9, 2011 in Tohoku using tsunami waveformsLearning from crustal deformation associated with the M9 2011 Tohoku-oki earthquakeThe slow earthquake spectrum in the Japan Trench illuminated by the S-net seafloor observatoriesA Decade of Lessons Learned from the 2011 Tohoku‐Oki EarthquakeLarge Coseismic Slip to the Trench During the 2011 Tohoku-Oki EarthquakeAlgorithms for the calculation of exact displacements, strains, and stresses for triangular dislocation elements in a uniform elastic half spaceA Self‐Consistent Fault Slip Model for the 2011 Tohoku Earthquake and TsunamiA review of the rupture characteristics of the 2011 Tohoku-oki Mw 9.1 earthquakeTrench-normal variation in observed seafloor displacements associated with the 2011 Tohoku-Oki earthquakeCoseismic slip distribution of the 2011 off the Pacific Coast of Tohoku Earthquake (M9.0) refined by means of seafloor geodetic dataCoseismic fault rupture at the trench axis during the 2011 Tohoku-oki earthquakeThe 2011 Tohoku-Oki Earthquake: Displacement Reaching the Trench AxisStress State in the Largest Displacement Area of the 2011 Tohoku-Oki EarthquakeLow Coseismic Friction on the Tohoku-Oki Fault Determined from Temperature MeasurementsRole of Weak Materials in Earthquake Rupture DynamicsEnergy‐Based Scenarios for Great Thrust‐Type Earthquakes in the Nankai Trough Subduction Zone, Southwest Japan, Using an Interseismic Slip‐Deficit ModelKinematic Barrier Constraints on the Magnitudes of Additional Great Earthquakes Off the East Coast of JapanShallow Dynamic Overshoot and Energetic Deep Rupture in the 2011 <i>M</i> <sub>w</sub> 9.0 Tohoku-Oki EarthquakeGeologically current plate motionsDisplacement Above the Hypocenter of the 2011 Tohoku-Oki EarthquakeInterplate seismogenic zones along the Kuril–Japan trench inferred from GPS data inversionRupture process of the 2011 Tohoku-oki earthquake and absolute elastic strain releaseLarge fault slip peaking at trench in the 2011 Tohoku-oki earthquakeTime and Space Distribution of Coseismic Slip of the 2011 Tohoku Earthquake as Inferred from Tsunami Waveform DataQuasi-Dynamic 3D Modeling of the Generation and Afterslip of a Tohoku-oki Earthquake Considering Thermal Pressurization and Frictional Properties of the Shallow Plate BoundarySlip‐Deficit Rate Distribution Along the Nankai Trough, Southwest Japan, With Elastic Lithosphere and Viscoelastic AsthenosphereUsing Tsunami Waves Reflected at the Coast to Improve Offshore Earthquake Source Parameters: Application to the 2016 Mw 7.1 Te Araroa Earthquake, New ZealandExtracting Near‐Field Seismograms From Ocean‐Bottom Pressure Gauge Inside the Focal Area: Application to the 2011 Mw 9.1 Tohoku‐Oki EarthquakeThe Generic Mapping Tools Version 6Solving Least Squares ProblemsImpulsive Tsunami and Large Runup Along the Sanriku Coast of Japan Produced by an Inelastic Wedge Deformation ModelConnection between high pore-fluid pressure and frictional instability at tsunamigenic plate boundary fault of 2011 Tohoku-Oki earthquakeCan the Updip Limit of Frictional Locking on Megathrusts Be Detected Geodetically? Quantifying the Effect of Stress Shadows on Near‐Trench CouplingMechanically Coupled Areas on the Plate Interface in the Nankai Trough, Japan and a Possible Seismic and Aseismic Rupture Scenario for Megathrust EarthquakesInverting for Slip on Three-Dimensional Fault Surfaces Using Angular Dislocations“Coupling” Semantics and science in earthquake researchThe State of Stress on the Fault Before, During, and After a Major EarthquakeFrictional properties of fault zone gouges from the J‐FAST drilling project (<i>M<sub>w</sub></i> 9.0 2011 Tohoku‐Oki earthquake)Tsunami Generation and PropagationLocating Fully Locked Asperities Along the South America Subduction Megathrust: A New Physical Interseismic Inversion Approach in a Bayesian FrameworkDepth‐varying rupture properties of subduction zone megathrust faultsGeodetic imaging of plate motions, slip rates, and partitioning of deformation in JapanInterplate coupling beneath NE Japan inferred from three‐dimensional displacement fieldA self‐consistent mechanism for slow dynamic deformation and tsunami generation for earthquakes in the shallow subduction zoneTsunami generation by horizontal displacement of ocean bottomTsunami earthquakes possibly widespread manifestations of frictional conditional stabilityStable creeping fault segments can become destructive as a result of dynamic weakeningDynamic Overshoot Near Trench Caused by Large Asperity Break at DepthStatic stress drop in the <i>M<sub>w</sub></i> 9 Tohoku‐oki earthquake: Heterogeneous distribution and low average valueLoci and maximum size of thrust earthquakes and the mechanics of the shallow region of subduction zonesThe Accumulation of Slip Deficit in Subduction Zones in the Absence of Mechanical Coupling: Implications for the Behavior of Megathrust EarthquakesTsunami waveform inversion incorporating permanent seafloor deformation and its application to tsunami forecastingCoseismic strengthening of the shallow portion of the subduction fault and its effects on wedge taperStructural characteristics off Miyagi forearc region, the Japan Trench seismogenic zone, deduced from a wide-angle reflection and refraction studyDynamic Wedge Failure and Along‐Arc Variations of Tsunamigenesis in the Japan Trench MarginThe postearthquake stress state on the Tohoku megathrust as constrained by reanalysis of the JFAST breakout dataA non-linear geodetic data inversion using ABIC for slip distribution on a fault with an unknown dip angleEarthquakes and friction lawsGeodetic data inversion using a Bayesian information criterion for spatial distribution of fault slipSpatial correlation of interseismic coupling and coseismic rupture extent of the 2011 M<sub>W</sub>= 9.0 Tohoku-oki earthquakeSlip rate deficit and earthquake potential on shallow megathrusts2011年東北地方太平洋沖地震による絶対歪みの解放：津波の第一波について : 津波の発生,伝播に関する古典的理論JAMSTEC Seismic Survey DatabaseOcean Tide Models Developed by Assimilating TOPEX/POSEIDON Altimeter Data into Hydrodynamical Model:A Global Model and a Regional Model around JapanAnomalous low velocity zone and linear alignment of seismicity along it in the Pacific slab beneath Kanto, Japan: reactivation of subducted fracture zone?Supplementary Dataset for "Extracting near-field seismograms from ocean-bottom pressure gauge inside the focal area: application to the 2011 Mw 9.1 Tohoku-Oki earthquake"Supplementary Dataset for "A new mechanical perspective on a shallow megathrust near-trench slip from the high- resolution fault model of the 2011 Tohoku-Oki earthquake"Seismicity near the hypocenter of the 2011 off the Pacific coast of Tohoku earthquake deduced by using ocean bottom seismographic dataSignificant tsunami observed at ocean-bottom pressure gauges during the 2011 off the Pacific coast of Tohoku EarthquakeCo- and postseismic slip behaviors extracted from decadal seafloor geodesy after the 2011 Tohoku-oki earthquakeOpenSWPC : an open-source integrated parallel simulation code for modeling seismic wave propagation in 3D heterogeneous viscoelastic media
- 連携機関・データベース
- 国立情報学研究所 : CiNii Research
- 提供元機関・データベース
- 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科学研究費助成事業データベース科学研究費助成事業データベースCrossrefCrossrefCrossrefCrossrefCrossrefCrossref
- 書誌ID（NDLBibID）
- 12998709