Rheological profile across the NE Japan interplate megathrust in the source region of the 2011 Mw9.0 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[10.1186/1880-5981-66-73]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
- Ichiko Shimizu
- 出版年月日等
- 2014-07-18
- 出版年（W3CDTF）
- 2014-07-18
- タイトル（掲載誌）
- EPS : Earth, Planets and Space
- 巻号年月日等（掲載誌）
- 66(73)
- 掲載巻
- 66(73)
- ISSN（掲載誌）
- 1880-5981
- ISSN-L（掲載誌）
- 1343-8832
- 本文の言語コード
- eng
- DOI
- 10.1186/1880-5981-66-73
- 国立国会図書館永続的識別子
- info:ndljp/pid/9227828
- 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）
- 2015-04-17T10:30:12+09:00
- 保存日（W3CDTF）
- 2014-10-10
- 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/9227755
- 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
- 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 > デジタル化資料 > 雑誌
- 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
- 所蔵機関
- 国立国会図書館
- 請求記号
- Z19-292
- 掲載誌（国立国会図書館永続的識別子）
- info:ndljp/pid/3427597
- 連携機関・データベース
- 国立国会図書館 : 国立国会図書館雑誌記事索引
- 書誌ID（NDLBibID）
- 9227828
- 整理区分コード
- 632
- 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
- 10.1186/1880-5981-66-73
- 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
- Special issue ‘Geofluid processes in subduction zones and mantle dynamics’Steady-State Microstructures of Quartz Revisited: Evaluation of Stress States in Deformation Experiments Using a Solid-Medium ApparatusExperimental grain growth of quartz aggregates under wet conditions and its application to deformation in natureTheoretical derivation of flow laws for quartz dislocation creep: Comparisons with experimental creep data and extrapolation to natural conditions using water fugacity correctionsFrictional Properties of Simulated Chlorite Gouge at Hydrothermal Conditions: Implications for Subduction Megathrusts
- 参照
- Megaquake cycle at the Tohoku subduction zone with thermal fluid pressurization near the surfacePotential tsunamigenic faults of the 2011 Tohoku earthquake3D modeling of the cycle of a great Tohoku-oki earthquake, considering frictional behavior at low to high slip velocitiesJoint inversion of strong motion, teleseismic, geodetic, and tsunami datasets for the rupture process of the 2011 Tohoku earthquakeFault lubrication during earthquakesLow Coseismic Shear Stress on the Tohoku-Oki Megathrust Determined from Laboratory ExperimentsOn the transient response of serpentine (antigorite) gouge to stepwise changes in slip velocity under high-temperature conditionsDetermination of the pore fluid pressure ratio at seismogenic megathrusts in subduction zones: Implications for strength of asperities and Andean‐type mountain buildingHydrogeology and Mechanics of Subduction Zone Forearcs: Fluid Flow and Pore PressureContinental fault structure and the shallow earthquake sourceStrength, porosity, and permeability development during hydrostatic and shear loading of synthetic quartz‐clay fault gougeCoseismic slip distribution of the 2011 off the Pacific Coast of Tohoku Earthquake (M9.0) refined by means of seafloor geodetic dataSubducted Seamount Imaged in the Rupture Zone of the 1946 Nankaido EarthquakeWeak Interplate Coupling by Seamounts and Repeating <i>M</i> ~ 7 EarthquakesTectonic erosion along the Japan and Peru convergent marginsAccretionary Complex Origin of the Mafic-Ultramafic Bodies of the Sanbagawa Belt, Central Shikoku, JapanGrain size reduction by dynamic recrystallization: can it result in major rheological weakening?Hydrologic controls on the morphology and mechanics of accretionary wedgesFriction on subduction megathrust faults: Beyond the illite–muscovite transitionAnomalous depth dependency of the stress field in the 2007 Noto Hanto, Japan, earthquake: Potential involvement of a deep fluid reservoirCompressional and shear wave velocities of serpentinized peridotites up to 200 MPaMechanics of fold‐and‐thrust belts and accretionary wedgesNew constraints on megathrust slip stability under subduction zone P – T conditionsFrictional slip of granite at hydrothermal conditionsThe eastern Tonale fault zone: a ‘natural laboratory’ for crystal plastic deformation of quartz over a temperature range from 250 to 700°CSpace–time distribution of interplate moment release including slow earthquakes and the seismo-geodetic coupling in the Sanriku-oki region along the Japan trenchEffect of aqueous and carbonic fluids on the dislocation creep strength of quartzPressure–temperature conditions of ongoing regional metamorphism beneath the Japanese IslandsInterplate seismogenic zones along the Kuril–Japan trench inferred from GPS data inversionWater distribution in low-grade siliceous metamorphic rocks by micro-FTIR and its relation to grain size: a case from the Kanto Mountain region, JapanStructural characteristics controlling the seismicity crustal structure of southern Japan Trench fore-arc region, revealed by ocean bottom seismographic dataA unified source model for the 2011 Tohoku earthquakeRupture process of the 2011 Tohoku-oki earthquake and absolute elastic strain releasePropagation of Slow Slip Leading Up to the 2011 <i>M</i> <sub>w</sub> 9.0 Tohoku-Oki EarthquakePore pressure distribution along plate interface that causes a shallow asperity of the 2011 great Tohoku-oki earthquakeAlong‐arc structural variation of the plate boundary at the Japan Trench margin: Implication of interplate couplingInterlocking of heterogeneous plate coupling and aftershock area expansion pattern for the 2011 Tohoku‐Oki Mw9 earthquakeDo subducting seamounts generate or stop large earthquakes?Thermal state under the Tohoko arc with consideration of crustal heat generationA rheologic model for wet crust applied to strike‐slip faultsStrength of the lithosphere: Constraints imposed by laboratory experimentsA constitutive scaling law and a unified comprehension for frictional slip failure, shear fracture of intact rock, and earthquake ruptureStructural controls on the Mw 9.0 2011 Offshore-Tohoku earthquakeSpatial heterogeneity of the mantle wedge structure and interplate coupling in the NE Japan forearc regionInfluence of subduction zone conditions and gouge composition on frictional slip stability of megathrust faultsExperimental deformation of flint in axial compressionNature of seismic coupling along simple plate boundaries of the subduction typeThe Serpentinite Multisystem Revisited: Chrysotile Is MetastablePhosphorus export across an urban to rural gradient in the Chesapeake Bay watershedA flow law for dislocation creep of quartz aggregates determined with the molten salt cellInversion for absolute deviatoric crustal stress using focal mechanisms and coseismic stress changes: The 2011 <i>M</i>9 Tohoku‐oki, Japan, earthquakeSlip distribution of the 1952 Tokachi‐Oki earthquake (<i>M</i> 8.1) along the Kuril Trench deduced from tsunami waveform inversionStrain geometries in the Sanbagawa Metamorphic Belt inferred from deformation structures in metabasiteTransition Between Frictional Slip and Ductile Flow for Halite Shear Zones at Room TemperatureMultimechanism friction constitutive model for ultrafine quartz gouge at hypocentral conditionsThe Asama igneous complex, central Japan: An ultramafic-mafic layered intrusion in the Mikabu greenstone belt, Sambagawa metamorphic terrainStrengths of serpentinite gouges at elevated temperaturesFriction in faulted rock at high temperature and pressureDirect observation of frictional contacts: New insights for state-dependent propertiesEffects of pressure on the micromechanics of faulting in San Marcos gabbroThe brittle-plastic transition and the depth of seismic faultingTheories and applicability of grain size piezometers: The role of dynamic recrystallization mechanismsExperimental intracrystalline plastic flow in hot-pressed synthetic quartzite prepared from Brazilian quartz crystalsStable creeping fault segments can become destructive as a result of dynamic weakeningInterplate earthquakes as a driver of shallow subduction erosionCommon depth of slab‐mantle decoupling: Reconciling diversity and uniformity of subduction zonesA significant relation between seismic activities and reflection intensities in the Japan Trench regionChapter 6. STRUCTURAL CHARACTERISTICS OF OPALINE AND MICROCRYSTALLINE SILICA MINERALSHigh pore pressures and porosity at 35 km depth in the Cascadia subduction zoneThrust-type subduction-zone earthquakes and seamount asperities: A physical model for seismic ruptureThe Mechanics of Earthquakes and FaultingComparison of smectite- and illite-rich gouge frictional properties: application to the updip limit of the seismogenic zone along subduction megathrustsThe brittle‐plastic transition in experimentally deformed quartz aggregatesAn evaluation of quartzite flow laws based on comparisons between experimentally and naturally deformed rocksDistribution of seismic coupling on the subducting plate boundary in northeastern Japan inferred from GPS observationsKinetics of pressure solution creep in quartz: theoretical considerationsUpper plate deformation associated with seamount subductionThe 2005 M7.2 MIYAGI‐OKI earthquake, NE Japan: Possible rerupturing of one of asperities that caused the previous M7.4 earthquakeTsunami earthquake generation by the release of gravitational potential energyPreparation and deformation of synthetic aggregates of quartzStructural characteristics off Miyagi forearc region, the Japan Trench seismogenic zone, deduced from a wide-angle reflection and refraction studyFriction of rocksFrictional sliding of gabbro gouge under hydrothermal conditionsCrustal stress field in southern California and its implications for fault mechanicsThe effect of seamount subduction on seismic couplingFault stability inferred from granite sliding experiments at hydrothermal conditionsRheology of synthetic anorthite‐diopside aggregates: Implications for ductile shear zones東日本太平洋沖地震後の余効変動解析へ向けた東北日本弧レオロジー断面Repeating earthquakes and quasi-static slip on the plate boundary east off northern Honshu, Japan関東山地三波川帯(低変成度地域)における流動変形Investigation of the earthquake sequence off Miyagi prefecture with historical seismogramsTransportation of H<sub>2</sub>O beneath the Japan arcs and its implications for global water circulationAsperity map along the subduction zone in northeastern Japan inferred from regional seismic dataStrong localized asperity of the 2011 Tohoku-Oki earthquake, JapanPossibility of Mw 9.0 mainshock triggered by diffusional propagation of after-slip from Mw 7.3 foreshockSpatial distribution and focal mechanisms of aftershocks of the 2011 off the Pacific coast of Tohoku EarthquakeA possible mechanism of M 9 earthquake generation cycles in the area of repeating M 7～8 earthquakes surrounded by aseismic slidingA complex rupture image of the 2011 off the Pacific coast of Tohoku Earthquake revealed by the MeSO-netCoseismic slip distribution of the 2011 off the Pacific coast of Tohoku Earthquake (M 9.0) estimated based on GPS data : was the asperity in Miyagi-oki ruptured？Coupling coefficient, hierarchical structure, and earthquake cycle for the source area of the 2011 off the Pacific coast of Tohoku earthquake inferred from small repeating earthquake dataNearly complete stress drop in the 2011 Mw 9.0 off the Pacific coast of Tohoku EarthquakeThe 2011 off the Pacific coast of Tohoku Earthquake related to a strong velocity gradient with the Pacific plateDetailed stress fields in the focal region of the 2011 off the Pacific coast of Tohoku Earthquake : implication for the distribution of moment release
- 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CrossrefCrossrefCrossrefCrossrefCrossref
- 書誌ID（NDLBibID）
- 9227828