Depth profile of frictional properties in the inner Nankai accretionary prism using cuttings from IODP Site C0002
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- 資料種別
- 記事
- 著者・編者
- Riho FujiokaIkuo KatayamaManami Kitamura
- 出版年月日等
- 2022-06-03
- 出版年（W3CDTF）
- 2022-06-03
- タイトル（掲載誌）
- Progress in earth and planetary science
- 巻号年月日等（掲載誌）
- 9(31)
- 掲載巻
- 9(31)
- 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/s40645-022-00488-1
- 国立国会図書館永続的識別子
- info:ndljp/pid/12307842
- 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）
- 2022-07-11T20:40:38+09:00
- 保存日（W3CDTF）
- 2022-07-11
- 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/s40645-022-00488-1
- 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
- Frictional properties of the décollement in the shallow Nankai Trough: Constraints from friction experiments simulating in-situ conditions and implications for the seismogenic zoneA review of shallow slow earthquakes along the Nankai Trough南海トラフにおける浅部スロー地震域の地質構造と摩擦特性
- 参照
- Connecting slow earthquakes to large earthquakesVery low frequency earthquakes within accretionary prisms are very low stress-drop earthquakesDynamic weakening of smectite‐bearing faults at intermediate velocities: Implications for subduction zone earthquakesHigh fluid-pressure patches beneath the décollement: a potential source of slow earthquakes in the Nankai Trough off Cape MurotoStrong sediments at the deformation front, and weak sediments at the rear of the Nankai accretionary prism, revealed by triaxial deformation experimentsStrength characteristics of Japan Trench borehole samples in the high-slip region of the 2011 Tohoku-Oki earthquakeShear strength of sediments approaching subduction in the Nankai Trough, Japan as constraints on forearc mechanicsPlate convergence and long‐term crustal deformation in central JapanComparison of frictional strength and velocity dependence between fault zones in the Nankai accretionary complexFriction experiments under in-situ stress reveal unexpected velocity-weakening in Nankai accretionary prism samplesFault rock heterogeneity can produce fault weakness and reduce fault stabilityVelocity-weakening friction induced by laboratory-controlled lithificationThe stabilizing effect of high pore-fluid pressure along subduction megathrust faults: Evidence from friction experiments on accretionary sediments from the Nankai TroughAbundance of smectite and the location of a plate-boundary fault, Barbados accretionary prismSource mechanisms and tectonic significance of historical earthquakes along the nankai trough, JapanA numerical simulation of earthquake cycles along the Nankai Trough in southwest Japan: lateral variation in frictional property due to the slab geometry controls the nucleation positionMechanical Weakness of the Nankai Accretionary Prism: Insights From <i>V</i><sub>p</sub> Measurements of Drill CuttingsFriction velocity dependence of clay-rich fault material along a megasplay fault in the Nankai subduction zone at intermediate to high velocitiesTsunamigenic potential of the shallow subduction plate boundary inferred from slow seismic slipShallow slow slip events along the Nankai Trough detected by GNSS-AHigh Pore Fluid Pressure May Cause Silent Slip in the Nankai TroughFriction experiments on saturated sediments and their implications for the stress state of the Nankai and Barbados subduction thrustsLithologic control of frictional strength variations in subduction zone sediment inputsRSFit3000: A MATLAB GUI-based program for determining rate and state frictional parameters from experimental dataEffective strength of incoming sediments and its implications for plate boundary propagation: Nankai and Costa Rica as type examples of accreting vs. erosive convergent marginsRecurring and triggered slow-slip events near the trench at the Nankai Trough subduction megathrustEffect of clay content and mineralogy on frictional sliding behavior of simulated gouges: Binary and ternary mixtures of quartz, illite, and montmorilloniteSeismic potential of weak, near-surface faults revealed at plate tectonic slip ratesSpatial Patterns in Frictional Behavior of Sediments Along the Kumano Transect in the Nankai Trough11. Friction of the Smectite Clay MontmorilloniteInfluence of subduction zone conditions and gouge composition on frictional slip stability of megathrust faultsFrictional properties of fault zone gouges from the J‐FAST drilling project (<i>M<sub>w</sub></i> 9.0 2011 Tohoku‐Oki earthquake)Slip instability and state variable friction lawsTemperature-dependent frictional properties of heterogeneous Hikurangi Subduction Zone input sediments, ODP Site 1124Modelling of short-interval silent slip events in deeper subduction interfaces considering the frictional properties at the unstable-stable transition regimeThe role of fault zone fabric and lithification state on frictional strength, constitutive behavior, and deformation microstructureConstitutive properties of clayey fault gouge from the Hanaore fault zone, southwest JapanUpdip limit of the seismogenic zone beneath the accretionary prism of southwest Japan: An effect of diagenetic to low-grade metamorphic processes and increasing effective stressEffect of hydration state on the frictional properties of montmorillonite‐based fault gougeFrictional behavior of large displacement experimental faultsGeodetic imaging of plate motions, slip rates, and partitioning of deformation in JapanDirect observation of frictional contacts: New insights for state-dependent propertiesSite C0002Frictional strength of wet and dry montmorilloniteLABORATORY-DERIVED FRICTION LAWS AND THEIR APPLICATION TO SEISMIC FAULTINGThe Mechanics of Earthquakes and FaultingComparison of smectite- and illite-rich gouge frictional properties: application to the updip limit of the seismogenic zone along subduction megathrustsModeling of rock friction: 1. Experimental results and constitutive equationsEpisodic slow slip events and rate‐and‐state frictionEarthquake nucleation in weak subducted carbonatesExpedition 358 summaryExperimental evidence linking slip instability with seafloor lithology and topography at the Costa Rica convergent marginSite C0002The effect of mineralogy and effective normal stress on frictional strength of sheet silicatesCompositional and fluid pressure controls on the state of stress on the Nankai subduction thrust: A weak plate boundaryEffects of humidity and interlayer cations on the frictional strength of montmorilloniteFrictional properties of the shallow Nankai Trough accretionary sediments dependent on the content of clay mineralsThree-dimensional topographic relief of the oceanic crust may control the occurrence of shallow very-low-frequency earthquakes in the Nankai Trough off KumanoCan clay minerals account for the behavior of non-asperity on the subducting plate interface？Frictional properties of sediments entering the Costa Rica subduction zone offshore the Osa Peninsula : implications for fault slip in shallow subduction zones
- 参照（URI）
- 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CrossrefCrossrefCrossref
- 書誌ID（NDLBibID）
- 12307842