Role of multiscale heterogeneity in fault slip from quasi-static numerical simulations
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DOI[10.1186/s40623-017-0676-5]のデータに遷移します
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- 資料種別
- 記事
- 著者・編者
- Hideo AochiSatoshi Ide
- 出版年月日等
- 2017-07-11
- 出版年(W3CDTF)
- 2017-07-11
- タイトル(掲載誌)
- EPS : Earth, Planets and Space
- 巻号年月日等(掲載誌)
- 69(94)
- 掲載巻
- 69(94)
- ISSN(掲載誌)
- 1880-5981
- ISSN-L(掲載誌)
- 1343-8832
- 本文の言語コード
- eng
- DOI
- 10.1186/s40623-017-0676-5
- 国立国会図書館永続的識別子
- info:ndljp/pid/10953822
- 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)
- 2017-09-14T21:01:06+09:00
- 保存日(W3CDTF)
- 2017-09-12
- 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(URI)
- 掲載誌(国立国会図書館永続的識別子)
- info:ndljp/pid/10319651
- 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/s40623-017-0676-5
- 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
- Stress-Breakdown Time and Slip-Weakening Distance Inferred from Slip-Velocity Functions on Earthquake FaultsLow Coseismic Shear Stress on the Tohoku-Oki Megathrust Determined from Laboratory ExperimentsScaling of earthquake rupture growth in the Parkfield area: Self‐similar growth and suppression by the finite seismogenic layerLarge nucleation before large earthquakes is sometimes skipped due to cascade‐up—Implications from a rate and state simulation of faults with hierarchical asperitiesSlip- and Time-dependent Fault Constitutive Law and its Significance in Earthquake Generation CyclesDynamic earthquake rupture modelled with an unstructured 3-D spectral element method applied to the 2011 M9 Tohoku earthquakeImpact of channel-like erosion patterns on the frequency–magnitude distribution of earthquakesDetermination of the friction law parameters of the Mw 6.7 Michilla earthquake in northern Chile by dynamic inversionPeriodic slow slip triggers megathrust zone earthquakes in northeastern JapanPropagation dynamics of seismic and aseismic slip governed by fault heterogeneity and Newtonian rheologyNonvolcanic Deep Tremor Associated with Subduction in Southwest JapanA large silent earthquake in the Guerrero seismic gap, MexicoGrowth of molten zone as a mechanism of slip weakening of simulated faults in gabbro during frictional meltingThrust‐type focal mechanisms of tectonic tremors in Taiwan: Evidence of subductionA slip pulse model with fault heterogeneity for low‐frequency earthquakes and tremor along plate interfacesCohesive force across the tip of a longitudinal-shear crack and Griffith's specific surface energyInterplate quasi‐static slip off Sanriku, NE Japan, estimated from repeating earthquakesSlip‐weakening behavior during the propagation of dynamic ruptures obeying rate‐ and state‐dependent friction lawsInterplate seismogenic zones along the Kuril–Japan trench inferred from GPS data inversionVariety and spatial heterogeneity of tectonic tremor worldwideLarge fault slip peaking at trench in the 2011 Tohoku-oki earthquakeSlip-dependent friction law and nucleation processes in earthquake ruptureFault constitutive relations inferred from the 2009‐2010 slow slip event in Guerrero, MexicoSeismic Evidence for an Earthquake Nucleation PhaseA constitutive scaling law and a unified comprehension for frictional slip failure, shear fracture of intact rock, and earthquake ruptureNumerical study on multi‐scaling earthquake ruptureConceptual and physical clarification of rate and state friction: Frictional sliding as a thermally activated rheologyDynamic inversion of the 2000 Tottori earthquake based on elliptical subfault approximationsForeshocks and pre‐events associated with the nucleation of large earthquakesSlip instability and state variable friction lawsScaling Relationships of Source Parameters for Slow Slip EventsWhich Dynamic Rupture Parameters Can Be Estimated from Strong Ground Motion and Geodetic Data?Depth‐varying rupture properties of subduction zone megathrust faultsPhenomenology of deep slow earthquake family in southwest Japan: Spatiotemporal characteristics and segmentationEarthquakes as multiscale dynamic ruptures with heterogeneous fracture surface energyModelling non-volcanic tremor, slow slip events and large earthquakes in the Guerrero subduction zone (Mexico) with space-variable frictional weakening and creepAseismic slip transients emerge spontaneously in three‐dimensional rate and state modeling of subduction earthquake sequencesEarthquake nucleation in intact or healed rocksOn the physical mechanism of silent slip events along the deeper part of the seismogenic zoneBridging the gap between seismically and geodetically detected slow earthquakesStable creeping fault segments can become destructive as a result of dynamic weakeningA slow earthquake sequence on the San Andreas faultTime-course gait analysis of hemiparkinsonian rats following 6-hydroxydopamine lesionNon-hypersingular boundary integral equations for 3-D non-planar crack dynamicsComplexity in earthquake sequences controlled by multiscale heterogeneity in fault fracture energySegmentation in episodic tremor and slip all along CascadiaComplex characteristics of slow slip events in subduction zones reproduced in multi‐cycle simulationsDetermination of constitutive relations of fault slip based on seismic wave analysisA cohesive zone model for dynamic shear faulting based on experimentally inferred constitutive relation and strong motion source parametersMechanism of deep low frequency earthquakes: Further evidence that deep non‐volcanic tremor is generated by shear slip on the plate interfaceDoes apparent stress vary with earthquake size?Three-Dimensional Dynamic Simulation of the 1992 Landers EarthquakeThree‐dimensional nonplanar simulation of the 1992 Landers earthquakeEpisodic tremor and slip on a frictional interface with critical zero weakening in elastic solidTowards inferring earthquake patterns from geodetic observations of interseismic couplingThe growth of slip surfaces in the progressive failure of over-consolidated claySlow Earthquakes Coincident with Episodic Tremors and Slow Slip EventsA Silent Slip Event on the Deeper Cascadia Subduction InterfaceModeling fast and slow earthquakes at various scales深部微動が明らかにする潮汐のプレート運動への影響Modeling Earthquakes Using Fractal Circular Patch Models with Lessons from the 2011 Tohoku-Oki EarthquakeConceptual multi-scale dynamic rupture model for the 2011 off the Pacific coast of Tohoku EarthquakeA scaling low for slow earthquakesA possible mechanism of M 9 earthquake generation cycles in the area of repeating M 7~8 earthquakes surrounded by aseismic slidingGround motions characterized by a multi-scale heterogeneous earthquake model
- 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
- 書誌ID(NDLBibID)
- 10953822