| scholarly article | Q13442814 |
| P819 | ADS bibcode | 1995JGR...10017587K |
| P356 | DOI | 10.1029/95JB01460 |
| P50 | author | David L. Kohlstedt | Q15437827 |
| Stephen J. Mackwell | Q26707089 | ||
| P2093 | author name string | Brian Evans | |
| P2860 | cites work | Transient creep in natural and synthetic, iron-bearing olivine single crystals: mechanical results and dislocation microstructures | Q23911840 |
| Creep Laws for the Mantle of the Earth [and Discussion] | Q29038512 | ||
| Venus: a contrast in evolution to Earth | Q38534480 | ||
| Seismic evidence for a lower-crustal detachment beneath san francisco bay, california | Q46047011 | ||
| Friction of rocks | Q55952349 | ||
| Fault Stress States, Pore Pressure Distributions, and the Weakness of the San Andreas Fault | Q56997478 | ||
| Conditions for the localization of deformation in pressure-sensitive dilatant materials | Q56997727 | ||
| Stick-slip as a mechanism for earthquakes | Q57141371 | ||
| The nature of the lower continental crust: Inferences from geophysics, surface geology, and crustal xenoliths | Q58042012 | ||
| Frictional constraints on thrust, wrench and normal faults | Q59048742 | ||
| Substantial hydrogen solubility in olivine and implications for water storage in the mantle | Q59076174 | ||
| An earthquake mechanism based on rapid sealing of faults | Q59089258 | ||
| Transition from cataclastic flow to dislocation creep of feldspar: Mechanisms and microstructures | Q59666224 | ||
| Solubility and diffusional uptake of hydrogen in quartz at high water pressures: Implications for hydrolytic weakening | Q59829840 | ||
| Chapter 19 Hydraulic Pulses in the Earth's Crust | Q59851300 | ||
| Porosity reduction and crustal pore pressure development | Q59851324 | ||
| Fault rocks and fault mechanisms | Q60680534 | ||
| On transient rheology and glacial isostasy | Q60715365 | ||
| A multiple-crack model of brittle fracture: 2. Time-dependent simulations | Q61000903 | ||
| A multiple-crack model of brittle fracture: 1. Non-time-dependent simulations | Q61000904 | ||
| Groundwater Flow in Low-Permeability Environments | Q61468442 | ||
| Rheology of olivine and the strength of the lithosphere | Q61635044 | ||
| Effects of temperature on friction: Constitutive equations and experiments with quartz gouge | Q63495947 | ||
| The brittle-ductile transition in a deformation-mechanism map for halite | Q63495959 | ||
| Limits on lithospheric stress imposed by laboratory experiments | Q97142243 | ||
| Scaling of ground motion parameters, state of stress, and focal depth | Q97855981 | ||
| Friction, overpressure and fault normal compression | Q98151072 | ||
| The role of water in the deformation of dunite | Q98962723 | ||
| High-temperature creep of olivine single crystals, 2. dislocation structures | Q107275074 | ||
| High-temperature creep of olivine single crystals 1. Mechanical results for buffered samples | Q107275406 | ||
| P433 | issue | B9 | |
| P921 | main subject | lithosphere | Q83296 |
| aquatic science | Q4782809 | ||
| P304 | page(s) | 17587-17602 | |
| P577 | publication date | 1995-09-10 | |
| P1433 | published in | Journal of Geophysical Research | Q2738009 |
| P1476 | title | Strength of the lithosphere: Constraints imposed by laboratory experiments | |
| P478 | volume | 100 |
| Q57884281 | A 19 to 17 Ma amagmatic extension event at the Mid-Atlantic Ridge: Ultramafic mylonites from the Vema Lithospheric Section |
| Q57851800 | A constitutive model for layer development in shear zones near the brittle-ductile transition |
| Q57851837 | A continuum mechanics model for normal faulting using a strain-rate softening rheology: implications for thermal and rheological controls on continental and oceanic rifting |
| Q97448123 | A dynamical model for generating Eurasian lithospheric stress and strain rate fields: Effect of rheology and cratons |
| Q61469883 | A mechanical model of the San Andreas fault and SAFOD Pilot Hole stress measurements |
| Q57877091 | A model for continental crust genesis by arc accretion: rare earth element evidence from the Irish Caledonides |
| Q57041694 | Afar triple junction triggered by plume-assisted bi-directional continental break-up |
| Q56288367 | Analogue experiments of propagation of oblique rifts |
| Q59789257 | Bias in estimates of lithosphere viscosity from interseismic deformation |
| Q96749835 | Block models of crustal motion in southern California constrained by GPS measurements |
| Q105248855 | Building the central Andes through axial lower crustal flow |
| Q58940136 | Burial and exhumation in a subduction wedge: Mutual constraints from thermomechanical modeling and natural P-T-t data (Schistes Lustrés, western Alps) |
| Q59853127 | Constraints from rocks in the Taiwan orogen on crustal stress levels and rheology |
| Q57533385 | Constraints on subducting plate strength within the Kermadec trench |
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| Q97484555 | Constrictional Strain and Linear Fabrics as a Result of Deformation Partitioning: A Multiscale Modeling Investigation and Tectonic Significance |
| Q98075965 | Creep events at the brittle ductile transition |
| Q59874964 | Creep of partially molten fine-grained gabbro under dry conditions |
| Q97447874 | Crustal structure beneath the eastern margin of the Tibetan Plateau and its tectonic implications |
| Q59796569 | Crustal structure of a transform plate boundary: San Francisco Bay and the central California continental margin |
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| Q59806755 | Evidence of fluid-filled upper crust from observations of postseismic deformation due to the 1992 Mw7.3 Landers earthquake |
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| Q97323427 | Evolutionary model of the Himalaya–Tibet system: geopoembased on new modelling, geological and geophysical data |
| Q61635008 | Experimental deformation of olivine single crystals at lithospheric temperatures |
| Q97868513 | Fault slip rates, effects of elastic heterogeneity on geodetic data, and the strength of the lower crust in the Salton Trough region, southern California |
| Q60704474 | Faulting processes controlled by the nonuniform thermal structure of the crust and uppermost mantle beneath the northeastern Japanese island arc |
| Q105242972 | Finite element modeling of short-wavelength folding on Venus: Implications for the plume hypothesis for crustal plateau formation |
| Q60326744 | Fluid flow and metasomatic fault weakening in the Moresby Seamount detachment, Woodlark Basin, offshore Papua New Guinea |
| Q106396738 | Frictional Strengths of Subduction Thrust Rocks in the Region of Shallow Slow Earthquakes |
| Q99517906 | Frictional-viscous flow of phyllosilicate-bearing fault rock: Microphysical model and implications for crustal strength profiles |
| Q107421769 | From microscope to mountain belt: 150 years of petrology and its contribution to understanding geodynamics, particularly the tectonics of orogens |
| Q107297128 | Generation of plate-like behavior and mantle heterogeneity from a spherical, viscoplastic convection model |
| Q60701429 | Geodetic and seismic constraints on some seismogenic zone processes in Costa Rica |
| Q57858216 | Geodynamic models of terrane accretion: Testing the fate of island arcs, oceanic plateaus, and continental fragments in subduction zones |
| Q97337342 | Geodynamics of synconvergent extension and tectonic mode switching: Constraints from the Sevier-Laramide orogen |
| Q59828262 | Global analysis of experimental data on the rheology of olivine aggregates |
| Q97448128 | Gravity influenced brittle-ductile deformation and growth faulting in the lithosphere during collision: Results from laboratory experiments |
| Q57879043 | Great earthquakes and slab pull: interaction between seismic coupling and plate–slab coupling |
| Q57855194 | Heterogeneous deformation in the Cascadia convergent margin and its relation to thermal gradient (Washington, NW USA) |
| Q59329363 | High Pressure Metamorphism Caused by Fluid Induced Weakening of Deep Continental Crust |
| Q58876159 | High-temperature embrittlement of extensional Alpine mylonite zones in the midcrustal ductile-brittle transition |
| Q57904477 | Imaging links between lithospheric architecture and surface geology in the Proterozoic Curnamona Province, Australia |
| Q57850236 | Implications of hydrostatic pore pressures and high crustal strength for the deformation of intraplate lithosphere |
| Q59805636 | Influence of lithosphere viscosity structure on estimates of fault slip rate in the Mojave region of the San Andreas fault system |
| Q97996614 | Interaction of strong lower and weak middle crust during lithospheric extension in western New Zealand |
| Q59966088 | Intraplate Strike-Slip Faulting, Stress Accumulation, and Shear Localization of a Crust-Upper Mantle System With Nonlinear Viscoelastic Material |
| Q97868452 | Lithospheric instability in obliquely convergent margins: San Gabriel Mountains, southern California |
| Q59712955 | Longevity and stability of cratonic lithosphere: Insights from numerical simulations of coupled mantle convection and continental tectonics |
| Q57662419 | Magma Ocean Cumulate Overturn and Its Implications for the Thermo-chemical Evolution of Mars |
| Q57851777 | Magmatic and tectonic extension at mid-ocean ridges: 1. Controls on fault characteristics |
| Q99233946 | Mantle flow distribution beneath the California margin |
| Q60146338 | Mantle upwelling and melting beneath slow spreading centers: effects of variable rheology and melt productivity |
| Q97484446 | Mechanical analyses of listric normal faulting with emphasis on seismicity assessment |
| Q57878983 | Modification of the lithospheric stress field by lateral variations in plate-mantle coupling |
| Q60714224 | Non-hotspot formation of volcanic chains: control of tectonic and flexural stresses on magma transport |
| Q98962721 | Nondilatant brittle deformation of serpentinites: Implications for Mohr-Coulomb theory and the strength of faults |
| Q59329513 | Normal faulting and viscous buckling in the Tibetan Plateau induced by a weak lower crust |
| Q97996611 | North American dynamics and western U.S. tectonics |
| Q92081277 | On the competing roles of fault reactivation and brittle failure in generating plate tectonics from mantle convection |
| Q60712557 | Outer rise stress changes related to the subduction of the Juan Fernandez Ridge, central Chile |
| Q107297127 | Planforms of self-consistently generated plates in 3D spherical geometry |
| Q100233493 | Plastic Faulting in Ice |
| Q97865289 | Poroelastic coupling between the 1992 Landers and Big Bear Earthquakes |
| Q38631556 | Porosity evolution at the brittle-ductile transition in the continental crust: Implications for deep hydro-geothermal circulation |
| Q59806710 | Postseismic deformation due to the Mw 6.0 2004 Parkfield earthquake: Stress-driven creep on a fault with spatially variable rate-and-state friction parameters |
| Q57880753 | Postseismic deformation following the 1999 Chi-Chi earthquake, Taiwan: Implication for lower-crust rheology |
| Q58391699 | Rayleigh-Taylor instability under a shear stress free top boundary condition and its relevance to removal of mantle lithosphere from beneath the Sierra Nevada |
| Q63947068 | Reassessing the Thermal Structure of Oceanic Lithosphere With Revised Global Inventories of Basement Depths and Heat Flow Measurements |
| Q46877748 | Reconciling surface plate motions with rapid three-dimensional mantle flow around a slab edge |
| Q58780061 | Reply [to “Comment on “SKS splitting beneath continental rifts zones” by Gao et al.”] |
| Q79438693 | Reservoir-induced deformation and continental rheology in vicinity of Lake Mead, Nevada |
| Q73312693 | Response of a Rheologically Stratified Lithosphere to Subduction of an Indenter‐Shaped Plate: Insights Into Localized Exhumation at Orogen Syntaxes |
| Q97484505 | Rheological control on the initial geometry of the Raft River detachment fault and shear zone, western United States |
| Q38310105 | Rheological decoupling at the Moho and implication to Venusian tectonics |
| Q60701331 | Rupture characteristics of the 2003 Mw 7.6 mid-Indian Ocean earthquake: Implications for seismic properties of young oceanic lithosphere |
| Q57866355 | Seismic anisotropy around subduction zones: Insights from three-dimensional modeling of upper mantle deformation and SKS splitting calculations |
| Q98962726 | Seismic evidence for broken oceanic crust in the 2004 Sumatra earthquake epicentral region |
| Q57098416 | Seismic evidence of a two-layer lithospheric deformation in the Indian Ocean |
| Q57879057 | Seismic tomography, surface uplift, and the breakup of Gondwanaland: Integrating mantle convection backwards in time |
| Q57853971 | Seismic-based estimate of hydraulic parameters at Vesuvius Volcano |
| Q58984237 | Sensitivity of earthquake cycles on the San Andreas fault to small changes in regional compression |
| Q107269101 | Sensitivity of the short- to intermediate-wavelength geoid to rheologic structure in subduction zones |
| Q59839221 | Short-scale variations of tectonic regimes in the western European stress province north of the Alps and Pyrenees |
| Q59370689 | Significance of strain localization in the lower crust for structural evolution and thermal history of metamorphic core complexes |
| Q107269107 | Simulating the thermochemical magmatic and tectonic evolution of Venus's mantle and lithosphere: Two-dimensional models |
| Q57879038 | Slab pull, slab weakening, and their relation to deep intra-slab seismicity |
| Q59712928 | Tectonic and thermal evolution of Venus and the role of volatiles: Implications for understanding the terrestrial planets |
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| Q59875606 | Tectonics, Dynamics, and Seismic Hazard in the Canada-Alaska Cordillera |
| Q102472687 | The Effects of Earthquakes and Fluids on the Metamorphism of the Lower Continental Crust |
| Q92081276 | The Quest for self-consistent generation of plate tectonics in mantle convection models |
| Q60714226 | The Relation between mantle dynamics and plate tectonics: A Primer |
| Q57865653 | The Significance of Heat Transport by Shallow Fluid Flow at an Active Plate Boundary: The Southern Alps, New Zealand |
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| Q59839223 | The deep crust of the Southern Rhine Graben: reflectivity and seismicity as images of dynamic processes |
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