Pages that link to "Item:Q54089"

The following pages link to David A Lockner (Q54089):

Displayed 50 items.

• Laboratory measurements of reservoir rock from the Geysers geothermal field, California (Q253806) ‎ (← links)
• Quantitative measure of the variation in fault rheology due to fluid-rock interactions (Q254496) ‎ (← links)
• Mineralogical characterization of protolith and fault rocks from the SAFOD Main Hole (Q254786) ‎ (← links)
• Strength recovery in quartzite is controlled by changes in friction in experiments at hydrothermal conditions up to 200°C (Q256890) ‎ (← links)
• Premonitory acoustic emissions and stick-slip in natural and smooth-faulted Westerly granite (Q256952) ‎ (← links)
• The transition from frictional sliding to shear melting in laboratory stick-slip experiments (Q257423) ‎ (← links)
• How geometrical constraints contribute to the weakness of mature faults (Q259076) ‎ (← links)
• Interaction between hydraulic fracture and a preexisting fracture under triaxial stress conditions (Q259189) ‎ (← links)
• Failure in laboratory fault models in triaxial tests (Q261978) ‎ (← links)
• Near-fault velocity spectra from laboratory failures and their relation to natural ground motion (Q263865) ‎ (← links)
• 32 - Rock failure and earthquakes (Q263929) ‎ (← links)
• Frictional slip of granite at hydrothermal conditions (Q266837) ‎ (← links)
• Undrained poroelastic response of sandstones to deviatoric stress change (Q268482) ‎ (← links)
• Effect of thermal and mechanical processes on hydraulic transmissivity evolution (Q269749) ‎ (← links)
• Is internal friction friction? (Q272522) ‎ (← links)
• Pressure solution and hydrothermal recrystallization of carbonate sediments - an experimental study - reply (Q274389) ‎ (← links)
• The effect of mineral bond strength and adsorbed water on fault gouge frictional strength (Q276697) ‎ (← links)
• A generalized law for brittle deformation of Westerly granite (Q276826) ‎ (← links)
• Hydrothermal minerals and microstructures in the Silangkitang geothermal field along the Great Sumatran fault zone, Sumatra, Indonesia (Q280204) ‎ (← links)
• Effects of smectite to illite transformation on the frictional strength and sliding stability of intact marine mudstones (Q280425) ‎ (← links)
• Crystallographic controls on the frictional behavior of dry and water-saturated sheet structure minerals (Q280550) ‎ (← links)
• Effect of clay content and mineralogy on frictional sliding behavior of simulated gouges: binary and ternary mixtures of quartz, illite, and montmorillonite (Q281635) ‎ (← links)
• Geometry of the Nojima fault at Nojima-Hirabayashi, Japan - I. A simple damage structure inferred from borehole core permeability (Q281968) ‎ (← links)
• Geometry of the Nojima fault at Nojima-Hirabayashi, Japan - II. Microstructures and their implications for permeability and strength (Q282056) ‎ (← links)
• Strength recovery and sealing under hydrothermal conditions (Q282877) ‎ (← links)
• Shear failure of a granite pin traversing a sawcut fault (Q283513) ‎ (← links)
• Weakening of peridotite sheared at hydrothermal conditions (Q283650) ‎ (← links)
• Electrical properties and anisotropy of schists and fault rocks from New Zealand’s Southern Alps under confining pressure (Q283976) ‎ (← links)
• Effects of temperature and sliding rate on frictional strength of granite (Q284007) ‎ (← links)
• Fault stability inferred from granite sliding experiments at hydrothermal conditions (Q284472) ‎ (← links)
• Role of fault gouge during Interaction between hydraulic fracture and a preexisting fracture (Q285183) ‎ (← links)
• Velocity anomalies: An alternative explanation based on data from laboratory experiments (Q286017) ‎ (← links)
• Physical modeling of the formation and evolution of seismically active fault zones (Q286035) ‎ (← links)
• Direct evidence for fluid pressure, dilatancy, and compaction affecting slip in isolated faults (Q286920) ‎ (← links)
• A geology and geodesy based model of dynamic earthquake rupture on the Rodgers Creek‐Hayward‐Calaveras Fault System, California (Q287275) ‎ (← links)
• Strengths of serpentinite gouges at elevated temperatures (Q287576) ‎ (← links)
• Stick slip, charge separation and decay (Q289330) ‎ (← links)
• Frictional strengths of talc-serpentine and talc-quartz mixtures (Q289685) ‎ (← links)
• The susceptibility of Oklahoma’s basement to seismic reactivation (Q291386) ‎ (← links)
• Strength of chrysotile-serpentinite gouge under hydrothermal conditions: Can it explain a weak San Andreas fault? (Q291549) ‎ (← links)
• Laboratory triggering of stick-slip events by oscillatory loading in the presence of pore fluid with implications for physics of tectonic tremor (Q292299) ‎ (← links)
• Hydraulic fracturing in granite under geothermal conditions (Q293080) ‎ (← links)
• Time-dependent weakening of granite at hydrothermal conditions (Q294600) ‎ (← links)
• Permeability reduction in granite under hydrothermal conditions (Q294756) ‎ (← links)
• KG²B, a collaborative benchmarking exercise for estimating the permeability of the Grimsel granodiorite - Part 2: modeling, microstructures and complementary data (Q295160) ‎ (← links)
• Frictional properties and 3-D stress analysis of the southern Alpine Fault, New Zealand (Q296069) ‎ (← links)
• A test of the double-shearing model of flow for granular materials (Q298420) ‎ (← links)
• Reduction of permeability in granite at elevated temperatures (Q298516) ‎ (← links)
• Microcrack interaction leading to shear fracture (Q298599) ‎ (← links)
• Pore fluid pressure, apparent friction, and Coulomb failure (Q305540) ‎ (← links)