Earthquake faulting in subduction zones : insights from fault rocks in accretionary prisms
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- 資料種別
- 記事
- 著者・編者
- Kohtaro UjiieGaku Kimura
- 出版年月日等
- 2014-05-09
- 出版年（W3CDTF）
- 2014-05-09
- タイトル（掲載誌）
- Progress in earth and planetary science
- 巻号年月日等（掲載誌）
- 1(7)
- 掲載巻
- 1(7)
- ISSN（掲載誌）
- 2197-4284
- ISSN-L（掲載誌）
- 2197-4284
- 本文の言語コード
- eng
- DOI
- 10.1186/2197-4284-1-7
- 国立国会図書館永続的識別子
- info:ndljp/pid/8752529
- 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）
- 2014-09-25T20:21:39+09:00
- 保存日（W3CDTF）
- 2014-08-04
- 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/8752522
- 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
- 10.1186/2197-4284-1-7
- オンライン閲覧公開範囲
- インターネット公開
- 参照
- Elastic interaction of parallel rate-and-state-dependent frictional faults with aging and slip laws: slow-slip faults can sometimes host fast eventsDetection of increased heating and estimation of coseismic shear stress from Raman spectra of carbonaceous material in pseudotachylytesEvidence of Localized Failure Along Altered Basaltic Blocks in Tectonic Mélange at the Updip Limit of the Seismogenic Zone: Implications for the Shallow Slow Earthquake SourceAn explanation for episodic tremor and slow slip constrained by crack-seal veins and viscous shear in subduction mélangeHigh‐velocity frictional strength across the Tohoku‐Oki megathrust determined from surface drilling torqueViscous strengthening followed by slip weakening during frictional melting of chertFrictional melting and thermal fracturing recorded in pelagic sedimentary rocks of the Jurassic accretionary complex, central JapanFrictional Strengths of Subduction Thrust Rocks in the Region of Shallow Slow EarthquakesDeformation Structures From Splay and Décollement Faults in the Nankai Accretionary Prism, SW Japan(IODP NanTroSEIZE Expedition 316): Evidence for Slow and Rapid Slip in Fault RocksMegathrust Shear Modulated by Albite Metasomatism in Subduction MélangesTomography of the source zone of the 2015 M 7.8 Nepal earthquakePelagic smectite as an important factor in tsunamigenic slip along the Japan TrenchLithification facilitates frictional instability in argillaceous subduction zone sedimentsStructure and lithology of the Japan Trench subduction plate boundary faultFor how long are pseudotachylytes strong? Rapid alteration of basalt-hosted pseudotachylytes from a shallow subduction complexComplete 40Ar resetting in an ultracataclasite by reactivation of a fossil seismogenic fault along the subducting plate interface in the Mugi Mélange of the Shimanto accretionary complex, southwest JapanVariations in stress and driving pore fluid pressure ratio using vein orientations along megasplay faults : Example from the Nobeoka Thrust, Southwest JapanThree‐dimensional texture of natural pseudotachylyte: Pseudotachylyte formation mechanism in hydrous accretionary complexPlate Interface Shear Zone in the Sanbagawa Metamorphic Belt, Constrained by RSCM Thermometry, U–Pb Zircon Dating and Phase Equilibria Modelling in the Sarutagawa Region, Central Shikoku, JapanQuasi-Dynamic 3D Modeling of the Generation and Afterslip of a Tohoku-oki Earthquake Considering Thermal Pressurization and Frictional Properties of the Shallow Plate BoundaryGeochemical analysis unveils frictional melting processes in a subduction zone faultDeformation and Material Transfer in a Fossil Subduction Channel: Evidence From the Island of Elba (Italy)Expedition 358 Preliminary Report: NanTroSEIZE Plate Boundary Deep Riser 4: Nankai Seismogenic/Slow Slip Megathrust東北地方太平洋沖地震後の緊急調査掘削（IODP第343次航海：J-FAST）の成果陸域断層の内部構造南海トラフ地震発生帯掘削がもたらした沈み込み帯の新しい描像A review by the chief editors of some of the most popular papers published by PEPS in 2014-2015
- 参照
- Trench-parallel anisotropy produced by serpentine deformation in dehydrated mantle wedgeLow 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 EarthquakeThe rheology of suspensions of solid particlesRheology of Suspensions in Polymeric LiquidsStretching of fluid inclusions in calcite as an indicator of frictional heating on faultsCoseismic fault rupture at the trench axis during the 2011 Tohoku-oki earthquakeThe 2011 Tohoku-Oki Earthquake: Displacement Reaching the Trench AxisLow Coseismic Friction on the Tohoku-Oki Fault Determined from Temperature MeasurementsSmectite to chlorite conversion by frictional heating along a subduction thrustNonvolcanic Deep Tremor Associated with Subduction in Southwest JapanPseudotachylytes in an ancient accretionary complex and implications for melt lubrication during subduction zone earthquakesOn the relation between fault strength and frictional stabilityInteractions between Temperature and Pore-Fluid Pressure during Earthquake Faulting and a Mechanism for Partial or Total Stress ReliefTsunamigenic potential of the shallow subduction plate boundary inferred from slow seismic slipShallow Dynamic Overshoot and Energetic Deep Rupture in the 2011 <i>M</i> <sub>w</sub> 9.0 Tohoku-Oki EarthquakeProgressive illitization in fault gouge caused by seismic slip propagation along a megasplay fault in the Nankai TroughPermeability anisotropy of serpentinite and fluid pathways in a subduction zoneEpisodic tremor and slow slip potentially linked to permeability contrasts at the MohoLow-frequency earthquakes in Shikoku, Japan, and their relationship to episodic tremor and slipDisplacement Above the Hypocenter of the 2011 Tohoku-Oki EarthquakeFrictional heating, fluid pressure, and the resistance to fault motionINVESTIGATION OF THE EFFECT OF HEAT ON THE CLAY MINERALS ILLITE AND MONTMORILLONITE*Fluidization of granular material in a subduction thrust at seismogenic depthsLarge amount of fluid migration around shallow seismogenic depth preserved in tectonic mélange: Yokonami mélange, the Cretaceous Shimanto Belt, Kochi, Southwest JapanSeismic slip propagation to the updip end of plate boundary subduction interface faults: Vitrinite reflectance geothermometry on Integrated Ocean Drilling Program NanTro SEIZE coresGeological and frictional aspects of very‐low‐frequency earthquakes in an accretionary prismStabilization of rapid frictional slip on a weakening fault by dilatant hardeningPrincipal Slip Zones in Limestone: Microstructural Characterization and Implications for the Seismic Cycle (Tre Monti Fault, Central Apennines, Italy)The thickness of subduction plate boundary faults from the seafloor into the seismogenic zoneRecognizing the seismic cycle along ancient faults: CO2-induced fluidization of breccias in the footwall of a sealing low-angle normal faultExperimental frictional heating of coal gouge at seismic slip rates: Evidence for devolatilization and thermal pressurization of gouge fluidsDynamical weakening of faults by acoustic fluidizationSlip weakening as a mechanism for slow earthquakesIllite-smectite patterns in sheared Pleistocene mudstones of the Southern Apennines and their implications regarding the process of illitization: A multiscale analysisThickness of the Seismic Slip ZonePseudotachylyte from an ancient accretionary complex: Evidence for melt generation during seismic slip along a master décollement?Deformation and hydrofracture in a subduction thrust at seismogenic depths: The Rodeo Cove thrust zone, Marin Headlands, CaliforniaOff‐scraping accretionary process under the subduction of young oceanic crust: The Shimanto Belt of Okinawa Island, Ryukyu ArcWhy the Brazil nuts are on top: Size segregation of particulate matter by shakingRheology of crystal‐bearing silicate melts: An experimental study at high viscositiesFrictional melting processes and products in geological materials: introduction and discussionComposite planar fabric of gouge from the Punchbowl Fault, CaliforniaFault structure, frictional properties and mixed-mode fault slip behaviorCo-seismic frictional melting along an out-of-sequence thrust in the Shimanto accretionary complex. Implications on the tsunamigenic potential of splay faults in modern subduction zonesThe crystal morphology of plagioclase feldspar produced during isothermal supercooling and constant rate cooling experimentsCoseismic fluid–rock interactions at high temperatures in the Chelungpu faultEarthquake faulting as a structural processStructural evolution of underthrusted sediments, Kodiak Islands, AlaskaHigh-VP/VS zone accompanying non-volcanic tremors and slow-slip events beneath southwestern 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 stressSlip zone and energetics of a large earthquake from the Taiwan Chelungpu-fault Drilling ProjectA physical basis for the frictional melting of some rock-forming mineralsDynamic changes in fluid redox state associated with episodic fault rupture along a megasplay fault in a subduction zoneViscosity of magmatic liquids: A modelComminution and fluidization of granular fault materials: implications for fault slip behaviorSuperheated friction-induced melts in zoned pseudotachylytes within the Adamello tonalites (Italian Southern Alps)Tectonic incorporation of the upper part of oceanic crust to overriding plate of a convergent margin: An example from the Cretaceous–early Tertiary Mugi Mélange, the Shimanto Belt, JapanRecord of mega-earthquakes in subduction thrusts: The black fault rocks of Pasagshak Point (Kodiak Island, Alaska)Mechanism of frictional fusion in fault zonesMicrostructural Development on Firing Illite and Smectite Clays Compared with that in KaoliniteEstimation of temperature rise in a shallow slip zone of the megasplay fault in the Nankai TroughRupture mechanism and interface separation in foam rubber models of earthquakes: a possible solution to the heat flow paradox and the paradox of large overthrustsStable creeping fault segments can become destructive as a result of dynamic weakeningThe seismogenic zone of subduction thrust faultsThe geologic record of deep episodic tremor and slipEffects of lithology, cataclasis and melting on the composition of fault-generated pseudotachylytes in Lewisian gneiss, ScotlandOn the mechanical role of smectite in subduction zonesEffects of frictional heating on the thermal, hydrologic, and mechanical response of a faultSliding behavior and deformation textures of heated illite gougeViscosity determinations of some frictionally generated silicate melts: Implications for fault zone rheology at high strain ratesIncrementally developed slickenfibers — Geological record of repeating low stress-drop seismic events?Observations of rapidly flowing granular-fluid materialsGeneration of Pseudotachylyte by Ancient Seismic FaultingMélange rheology and seismic styleA review of recent developments concerning the structure, mechanics and fluid flow properties of fault zonesViscosities of magmatic silicate liquids; an empirical method of predictionComparison of smectite- and illite-rich gouge frictional properties: application to the updip limit of the seismogenic zone along subduction megathrustsExperiments on a gravity-free dispersion of large solid spheres in a Newtonian fluid under shearAn empirical equation of the relative viscosity of polymer melts filled with various inorganic fillersEpisodic Tremor and Slip on the Cascadia Subduction Zone: The Chatter of Silent SlipThe depth of seismic faulting and the upper transition from stable to unstable slip regimesHigh‐velocity frictional properties of gabbroWarm fluid migration along tectonic melanges in the Kodiak Accretionary Complex, AlaskaThe updip and downdip limits to great subduction earthquakes: Thermal and structural models of Cascadia, south Alaska, SW Japan, and ChileBrecciation processes in fault zones: Inferences from earthquake rupturingLarge-scale pseudotachylytes and fluidized cataclasites from an ancient subduction thrust faultDilatancy, compaction, and slip instability of a fluid‐infiltrated faultMicrostructural and chemical changes associated with cataclasis and frictional melting at shallow crustal levels: the cataclasite-pseudotachylyte connectionHigh-velocity frictional behavior and microstructure evolution of fault gouge obtained from Nojima fault, southwest JapanCan pseudotachylytes be used to infer earthquake source parameters? An example of limitations in the study of exhumed faultsShear veins observed within anisotropic fabric at high angles to the maximum compressive stressSlow Earthquakes Coincident with Episodic Tremors and Slow Slip EventsA scaling low for slow earthquakes
- 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CrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossref
- 書誌ID（NDLBibID）
- 8752529