記事
Friction of rocks
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CiNii Research
Friction of rocks
- 資料種別
- 記事
- 著者
- J. Byerlee
- 出版者
- Springer Science and Business Media LLC
- 出版年
- 1978-07
- 資料形態
- デジタル
- 掲載誌名
- pure and applied geophysics 116 4-5
- 掲載ページ
- p.615-626
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デジタル
- 資料種別
- 記事
- 著者標目
- 出版年月日等
- 1978-07
- 出版年（W3CDTF）
- 1978-07
- タイトル（掲載誌）
- pure and applied geophysics
- 巻号年月日等（掲載誌）
- 116 4-5
- 掲載巻
- 116
- 掲載号
- 4-5
- 掲載ページ
- 615-626
- 掲載年月日（W3CDTF）
- 1978-07
- ISSN（掲載誌）
- 00334553
- 出版事項（掲載誌）
- Springer Science and Business Media LLC
- 対象利用者
- 一般
- DOI
- 10.1007/bf00876528
- 作成日（W3CDTF）
- 2004-12-24
- 著作権情報
- https://www.springernature.com/gp/researchers/text-and-data-mining
- 関連情報（URI）
- 参照
- Propagation of Coulomb stress uncertainties in physics‐based aftershock modelsWhich is heterogeneous, stress or strength? An estimation from high-density seismic observationsTemporal changes in the internal stresses and pore pressures in a large-scale submarine mass transport depositThree-dimensional numerical modeling of temperature and mantle flow fields associated with subduction of the Philippine Sea plate, southwest JapanSubduction thermal regime, slab dehydration, and seismicity distribution beneath Hikurangi based on 3-D simulationsTemperature distribution for interplate seismic events in the southcentral Alaska subduction zone based on 3-D thermomechanical modelingRelationship of evolution of slip-surface structure in Indian sandstone to changes in friction coefficient for a wide range of slip ratesPrestate of Stress and Fault Behavior During the 2016 Kumamoto Earthquake (<i>M</i>7.3)Elastic strain energy and pore-fluid pressure control of aftershocksGeometrical dependence on the stress and slip tendency acting on the subduction megathrust of the Nankai seismogenic zone off KumanoThe effective stress law at a brittle‐plastic transition with a halite gouge layerHomoclinic bifurcation of a rate-weakening patch in a viscoelastic medium and effect of strength contrastStable Forearc Stressed by a Weak Megathrust: Mechanical and Geodynamic Implications of Stress Changes Caused by the M = 9 Tohoku‐Oki EarthquakeSteady‐State Effective Normal Stress in Subduction Zones Based on Hydraulic Models and Implications for Shallow Slow EarthquakesThree-dimensional thermomechanical modelling beneath Guerrero, Mexico, and its relation to the occurrence of interplate seismic phenomenaNear-trench slip potential of megaquakes evaluated from fault properties and conditions.Coulomb stress change on inland faults during megathrust earthquake cycle in southwest JapanRoughness Evaluation for Distinguishing Fresh and Sheared Rock Joint Surfaces with Different Sampling Intervals3-D thermal regime and dehydration processes around the regions of slow earthquakes along the Ryukyu TrenchThe role of fluids in earthquake swarms in northeastern Noto Peninsula, central Japan: insights from source mechanismsSpine growth and seismogenic faulting at Mt. Unzen, JapanInteraction among alluvial cover, bed roughness, and incision rate in purely bedrock and alluvial‐bedrock channelEnergy partition for grain crushing in quartz gouge during subseismic to seismic fault motion: An experimental studyLocalized rotation of principal stress around faults and fractures determined from borehole breakouts in hole B of the Taiwan Chelungpu-fault Drilling Project (TCDP)High fluid pressure and triggered earthquakes in the enhanced geothermal system in Basel, SwitzerlandFault lubrication during earthquakesExtreme hydrothermal conditions at an active plate-bounding faultLow Coseismic Shear Stress on the Tohoku-Oki Megathrust Determined from Laboratory ExperimentsSuppression of slip and rupture velocity increased by thermal pressurization: Effect of dilatancyDisplacement and dynamic weakening processes in smectite‐rich gouge from the Central Deforming Zone of the San Andreas FaultEvolution of pore fluid pressures in a stimulated geothermal reservoir inferred from earthquake focal mechanismsAnisotropic Horizontal Thermal Contraction of Young Oceanic Lithosphere Inferred From Stress Release Due To Oceanic Intraplate EarthquakesStrong sediments at the deformation front, and weak sediments at the rear of the Nankai accretionary prism, revealed by triaxial deformation experimentsVoids and Rock Friction at Subseismic Slip VelocityA frictional law for volcanic ash gougeStrength characteristics of Japan Trench borehole samples in the high-slip region of the 2011 Tohoku-Oki earthquakeThe relative timing of Lunar Magma Ocean solidification and the Late Heavy Bombardment inferred from highly degraded impact basin structuresA computerized method to estimate friction coefficient from orientation distribution of meso-scale faultsSpatial distribution of stress and frictional strength along the interplate boundary in northern Japan and its correlation to the locations of large earthquakesEffects of pore fluid pressure and tectonic stress on diverse seismic activities around the Mt. Ontake volcano, central JapanAbsolute Stress Fields in the Source Region of the 1992 Landers EarthquakeRecognition of shear heating on a long‐lived major fault using Raman carbonaceous material thermometry: implications for strength and displacement history of the MTL, SW JapanAlong-strike variations in temperature and tectonic tremor activity along the Hikurangi subduction zone, New ZealandEvolution of the rheological structure of MarsEffects of humidity and interlayer cations on the frictional strength of montmorilloniteCoseismic Slip Distribution of the 2 July 2013 Mw 6.1 Aceh, Indonesia, Earthquake and Its Tectonic ImplicationsFault model of the 2012 doublet earthquake, near the up-dip end of the 2011 Tohoku-Oki earthquake, based on a near-field tsunami: implications for intraplate stress statePressure‐to‐Depth Conversion Models for Metamorphic Rocks: Derivation and ApplicationsShear strength of a shear zone in the brittle-plastic transition based on tensorial strain partitioningThree‐Dimensional Pore Fluid Pressures in Source Region of 2017 Pohang Earthquake Inferred From Earthquake Focal MechanismsSlow Stick‐Slip Failure in Halite Gouge Caused by Brittle‐Plastic Fault HeterogeneityThe effect of a gouge layer on rupture propagation along brittle shear fractures in deep and high-stress minesSpatiotemporal Change in the Stress State Around the Hypocentral Area of the 2016 Kumamoto Earthquake SequenceFrictional stability of porous tuff breccia under subsurface pressure conditions and implications for shallow seismicityLong‐Living Earthquake Swarm and Intermittent Seismicity in the Northeastern Tip of the Noto Peninsula, JapanA small amount of water reduces the friction of the preferentially oriented montmorillonite gougeLow-temperature friction experiments on ice–salt mixtures: Implications for the strength of ice plate boundaries on EuropaThe stabilizing effect of high pore-fluid pressure along subduction megathrust faults: Evidence from friction experiments on accretionary sediments from the Nankai TroughFault strength, healing and stability in the Nankai Trough accretionary prism off Kii Peninsula, Japan, as illustrated by friction experiments on gouge of a cored sampleFault rock properties and conditions produce variance in slip during earthquake rupture propagation at the Nankai TroughChanges in seismic activity following the 2011 Tohoku-oki earthquake: Effects of pore fluid pressurePossible mechanism of mud volcanism at the prism-backstop contact in the western Mediterranean Ridge Accretionary ComplexLithification facilitates frictional instability in argillaceous subduction zone sedimentsLow Coseismic Friction on the Tohoku-Oki Fault Determined from Temperature MeasurementsRheological profile across the NE Japan interplate megathrust in the source region of the 2011 Mw9.0 Tohoku-oki earthquakeAdhesion energy between mica surfaces: Implications for the frictional coefficient under dry and wet conditionsChanges in the stress field after the 2008 <i>M</i>7.2 Iwate‐Miyagi Nairiku earthquake in northeastern JapanGraphite as a lubricating agent in fault zones: An insight from low‐ to high‐velocity friction experiments on a mixed graphite‐quartz gougeHigh-velocity frictional behavior of Longmenshan fault gouge from Hongkou outcrop and its implications for dynamic weakening of fault during the 2008 Wenchuan earthquakeStick–slip behavior of Indian gabbro as studied using a NIED large-scale biaxial friction apparatusTwo-dimensional thermal modeling of subduction of the Philippine Sea plate beneath southwest JapanDetermining changes in the state of stress associated with an earthquake via combined focal mechanism and moment tensor analysis: Application to the 2013 Awaji Island earthquake, JapanDepth-dependent stress field in and around the Atotsugawa fault, central Japan, deduced from microearthquake focal mechanisms: Evidence for localized aseismic deformation in the downward extension of the faultAn inhomogeneous across-slab conduit controlled by intraslab stress heterogeneity in the Nankai subduction zoneRelationship between temperatures and fault slips on the upper surface of the subducting Philippine Sea plate beneath the Kanto district, central JapanRole of Weak Materials in Earthquake Rupture DynamicsInelastic behavior and mechanical strength of the shallow upper crust controlled by layer-parallel slip in the high-strain zone of the Niigata region, JapanFor how long are pseudotachylytes strong? Rapid alteration of basalt-hosted pseudotachylytes from a shallow subduction complexRheology of the Fluid Oversaturated Fault Zones at the Brittle‐Plastic TransitionMechanical characterisation of new Sand-Hemihydrate rock-analogue material: Implications for modelling of brittle crust processesCaldera collapse thresholds correlate with magma chamber dimensionsConstraint on the background stress in the source region of the 2016 Kumamoto earthquake sequence based on temporal changes in elastic strain energies and coseismic stress rotationSpatial variation in stress orientation in and around Türkiye: rupture propagation across the stress regime transition in the 2023 <i>M</i>w 7.8 Kahramanmaraş earthquakeInterlayer bonding energy of layered minerals: Implication for the relationship with friction coefficientEffects of water transportation on subduction dynamics: Roles of viscosity and density reductionEffect of water on weakening preceding rupture of laboratory‐scale faults: Implications for long‐term weakening of crustal faultsFrictional characteristics of single and polycrystalline muscovite and influence of fluid chemistryLong‐Term Stability of Plate‐Like Behavior Caused by Hydrous Mantle Convection and Water Absorption in the Deep MantleDynamics of Subducting Slabs: Numerical Modeling and Constraints from Seismology, Geoid, Topography, Geochemistry, and PetrologyShear-induced graphitization of carbonaceous materials during seismic fault motion: Experiments and possible implications for fault mechanicsReduction in BET surface area of Nojima fault gouge with seismic slip and its implication for the fracture energy of earthquakesRelationships among temperature, dehydration of the subducting Philippine Sea plate, and the occurrence of a megathrust earthquake, low-frequency earthquakes, and a slow slip event in the Tokai district, central JapanExtremely weak fault planes: An estimate of focal mechanisms from stationary seismic activity in the San'in district, JapanFrictional experiments of dolerite at intermediate slip rates with controlled temperature: Rate weakening or temperature weakening?Emplacement mechanism of off‐axis large submarine lava field from the Oman OphioliteCarbon-forming reactions under a reducing atmosphere during seismic fault slipHeterogeneity in friction strength of an active fault by incorporation of fragments of the surrounding host rockOverpressurized fluids drive microseismic swarm activity around Mt. Ontake volcano, JapanSensitivity of elastic thickness to water in the Martian lithosphereStrength models of the terrestrial planets and implications for their lithospheric structure and evolutionLocalized fluid discharge by tensile cracking during the post-seismic period in subduction zonesNew granular rock-analogue materials for simulation of multi-scale fault and fracture processesFrictional properties of the décollement in the shallow Nankai Trough: Constraints from friction experiments simulating in-situ conditions and implications for the seismogenic zoneCyclic fracturing during spine extrusion at Unzen volcano, JapanMining-induced fault failure and coseismic slip based on numerical investigationDynamics of slab rollback and induced back-arc basin formationDynamic modeling of slow slip coupled with tremorFlash weakening is limited by granular dynamicsStress rotations and the long-term weakness of the Median Tectonic Line and the Rokko-Awaji SegmentRunaway slip to the trench due to rupture of highly pressurized megathrust beneath the middle trench slope: The tsunamigenesis of the 2011 Tohoku earthquake off the east coast of northern JapanWhy primordial continents were recycled to the deep: Role of subduction erosionRaman spectra of carbonaceous materials in a fault zone in the Longmenshan thrust belt, China; comparisons with those of sedimentary and metamorphic rocksScale dependence of rock friction at high work ratePore pressure distribution in the focal region of the 2008 M7.2 Iwate-Miyagi Nairiku earthquakeFrictional properties of sediments entering the Costa Rica subduction zone offshore the Osa Peninsula: implications for fault slip in shallow subduction zonesShear strain concentration mechanism in the lower crust below an intraplate strike-slip fault based on rheological laws of rocksInitiation of plate tectonics in the Hadean: Eclogitization triggered by the ABEL BombardmentDeformation of mafic schists from subducted oceanic crust at high pressure and temperature conditionsStress and pore fluid pressure control of seismicity rate changes following the 2016 Kumamoto earthquake, JapanSemi-brittle deformation of antigorite serpentinite under forearc mantle wedge conditionsAtomic-scale interlayer friction of gibbsite is lower than brucite due to interactions of hydroxylsSlab-derived fluid storage in the crust elucidated by earthquake swarmPotential Role of Volcanic Glass‐Smectite Mixtures in Slow Earthquakes in Shallow Subduction Zones: Insights From Low‐ to High‐Velocity Friction ExperimentsFault strength and rupture process controlled by fault surface topographyThermoelastic instability on a frictional surface and its implication for size effect in friction experimentsSpatial and Temporal Stress Variations before and after the 2008 Wenchuan <i>M</i><sub>w</sub> 7.9 Earthquake and its Implications: A Study based on Borehole Stress DataTwo‐Dimensional Thermal Modeling of the Philippine Sea Plate Subduction in Central Japan: Implications for Gap of Low‐Frequency Earthquakes and Tectonic TremorsThe 3‐D Spatial Distribution of Shear Strain Energy Changes Associated With the 2016 Kumamoto Earthquake Sequence, Southwest JapanDynamic Modelling of Induced Seismicity by Using Seismic Efficiency Constraints and a New Scaling Law for Slip-Weakening DistanceInterlayer energy of pyrophyllite: Implications for macroscopic frictionFirst‐principles Investigation of Frictional Characteristics of Brucite: An Application to Its Macroscopic Frictional CharacteristicsDiagenetic and shear-induced transitions of frictional strength of carbon-bearing faults and their implications for earthquake rupture dynamics in subduction zones勇払油ガス田におけるジオメカニクスによる生産性フラクチャーの評価INFLUENCE OF FAULT MECHANISM, DEPTH, AND REGION ON STRESS DROPS OF SMALL AND MODERATE EARTHQUAKES IN JAPAN間隙水圧・変形連成問題への最近の取り組み 花崗岩を起源とする断層ガウジの剪断強度および水理特性確率論的断層変位ハザード解析の信頼性向上逆断層による応力場と関連する地震活動Elastic property of damaged zone inferred from in-situ stresses and its role on the shear strength of faultsOrigin of the concentrated deformation zone in the Japanese Islands and stress accumulation process of intraplate earthquakes近年の地震観測により得られた東北日本の応力場の不均質性と断層強度および地震発生機構の関係蛇紋岩の力学的性質とそのテクトニックな意義岩床粗度と砂礫被覆に関する実験的研究APPLICABILITY OF SLIP TENDENCY FOR UNDERSTANDING LONG-TERM FAULT ACTIVITY: A CASE STUDY OF ACTIVE FAULTS IN NORTHEASTERN JAPANRETRACTED: Is the plastic flow uniformly distributed below the seismogenic region?Off-fault aftershocks of the 2005West Off Fukuoka Prefecture Earthquake: Reactivation of a structural boundary?A new view of earthquake and volcano precursorsThe Indo–Eurasia convergent margin and earthquakes in and around Tibetan Plateau要素内で閉じる付加自由度を用いた拡張有限要素法による斜面の動的破壊解析断層帯と断層レオロジーの進化
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